Journal articles on the topic 'Strada Reale'
To see the other types of publications on this topic, follow the link: Strada Reale.
Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles
Consult the top 50 journal articles for your research on the topic 'Strada Reale.'
Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.
You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.
Browse journal articles on a wide variety of disciplines and organise your bibliography correctly.
1
Revello Lami, Martina. "La complessitá del reale e la sua immagine." Ex Novo: Journal of Archaeology 5 (May 24, 2021): 145–52. http://dx.doi.org/10.32028/exnovo.v5i.415.
Full textAbstract:
Nato a Lucca nel 1981, Daniele si appassiona al disegno e all'arte già da bambino. Interrotto il cammino scolastico affascinato dalle sottoculture giovanili e dai codici suburbani si é dedicato allo studio ed alla pratica del tatuaggio, mestiere che ha praticato per 20 anni e che gli ha dato l’opportunitá di viaggiare in Europa e nel mondo per assorbire tutti gli stimoli e le ispirazioni possibili. La necessità di ampliare il suo raggio d’azione, esprimere concetti complessi attraverso la sua arte, trovare la strada della descrizione della realtà e dare vita ad un percorso artistico piú completo portano Daniele a calarsi sempre più spesso nei panni del pittore. Partendo dagli acquerelli, dal paesaggio al ritratto, ed approdato infine all'olio, la sua arte è una personale lettura della complessità del mondo.
2
Matteucci, Ivana. "Personal network e comunità ibride: le social street." SOCIOLOGIA URBANA E RURALE, no. 125 (August 2021): 97–115. http://dx.doi.org/10.3280/sur2021-125006.
Full textAbstract:
Questo articolo intende verificare come il personal network generato nello spazio online tramite l'appartenenza ai gruppi social e alle comunità virtuali, rappresenti un contributo e un supporto alla vita relazionale del soggetto nello spazio sociale reale. É stato compiuto uno studio esplorativo dove, attraverso l'analisi di un caso, sono state gettate le basi interpretative per la comprensione del fenomeno delle Social Street, che in future ricerche potranno essere testate su un numero più ampio di casi. Con il metodo del questionario online sono stati coinvolti alcuni iscritti a un gruppo Facebook di una Social Street. Si è trovato che la vita comunitaria online dei soggetti può essere significativamente connessa alla vita offline del gruppo nello spazio sociale urbano condiviso costituito dalla strada, configurando il nostro esempio come comunità ibrida e caso concreto di realtà aumentata.
3
Caianiello, Michele. "Processo penale e prescrizione nel quadro della giurisprudenza europea. Dialogo tra sistemi o conflitto identitario?" Revista Brasileira de Direito Processual Penal 3, no. 3 (October 14, 2017): 967. http://dx.doi.org/10.22197/rbdpp.v3i3.99.
Full textAbstract:
Precarietà e incertezza sembrano affliggere, nei tempi recenti, la prescrizione del reato, quando la si osservi da una prospettiva sovranazionale o comparata. Sullo sfondo, si pone il problema della tenuta del nostro sistema nel suo complesso, e persino della sua identità, come l’abbiamo concepita e tramandata di generazione in generazione. Con l’ordinanza n. 24 del 2017, la Corte costituzionale, sollevando una nuova questione pregiudiziale, mostra l’intento di non consumare una rottura del dialogo con l’ordinamento UE, limitandosi a paventare il rischio di ricorrere ai controlimiti, senza effettivamente porli in essere. Tuttavia, il provvedimento appare criticabile per alcuni argomenti utilizzati, e per la posizione assunta, che sembra lasciare poco spazio per specificazioni e aggiustamenti alla Corte di giustizia. La decisione, infatti, pur mostrando formalmente apertura a un confronto con la Corte di giustizia, tende a proporre in realtà una divisione tra mondi opposti e inconciliabili: di qua il diritto italiano, con la sua tradizione irrinunciabile; di là quello europeo, al quale formalmente si mostra deferenza (purché non si ingerisca in questioni vitali). Sembra il piano per una sorta di convivenza da separati, che certo ha il pregio di guadagnare tempo. Tuttavia, non si intravvede, nel ragionamento condotto, alcuna strada per raggiungere, o almeno per intraprendere il cammino verso una integrazione reale degli ordinamenti: è questo, in realtà, il nodo che, se non affrontato adesso, tenderà a riproporsi in successive occasioni.
4
Fiori, Angelo, and Lea Cinzia Caprioli. "La fecondazione artificiale eterologa: un altro ritorno al matrilineare?" Medicina e Morale 43, no. 2 (April 30, 1994): 213–30. http://dx.doi.org/10.4081/mem.1994.1019.
Full textAbstract:
Gli Autori, dopo un breve ricordo storico-antropologico delle primitive società matrilineari, passano in rassegna le principali legislazioni internazionali riguardanti le tecniche di procreazione artificiale, puntando l'attenzione sulle norme circa il riconoscimento di paternità legale al marito o convivente che ha prestato il proprio consenso alla fecondazione artificiale eterologa e circa l'anonimato del donatore di seme. Essi rilevano la contraddizione tra le attuali possibilità della ricerca biologica di paternità che, avvalendosi degli accertamenti genetici basati sull'impiego dei polimorfismi del sangue, consente a chiunque di conoscere il proprio padre biologico, e le norme sull'anonimato che, non consentendo al figlio di conoscere il proprio vero padre, creano notevoli diseguaglianze tra cittadini. La fecondazione artificiale eterologa viene considerata come un altro regresso alla società matrilineare, in cui la struttura protofamiliare era incentrata sulla figura della donna, la quale assumeva un ruolo dominante come strumento di fecondità e il "marito" era "in visita", cosicché padre e figlio erano completamente estranei l'uno all'altro. Viene infine commentata la recente sentenza del Tribunale di Cremona che ha accolto l'istanza di disconoscimento di paternità di un figlio nato a seguito di inseminazione artificiale con sperma eterologo. Il Tribunale, mancando in Italia una legge che regoli la fecondazione artificiale eterologa, ha percorso l'unica strada a disposizione nell'attuale panorama giuridico nazionale, fondando la propria sentenza sugli art t. 231 , 235 c 143 del Codice Civile. L'auspicio è che storie come quelle del piccolo Mattia, oggi "figlio di padre ignoto", inducano tutti a riflettere sui "prodigi" della scienza e del progresso, ma soprattutto non spingano frettolosamente verso leggi che consentano, per la loro permissività, di sconvolgere la reale biologia dell'essere umano.
5
Holloway, David J., and Juan J. Rustán. "The trilobite Reedops (Phacopidae) in the Lower Devonian of Argentina (Malvinokaffric Realm)." Journal of Paleontology 86, no. 2 (March 2012): 253–57. http://dx.doi.org/10.1666/11-082.1.
Full textAbstract:
The trilobite Reedops is documented from strata probably corresponding to the middle part of the Talacasto Formation in the Sierra de las Minitas, at the northernmost extent of the Precordillera in La Rioja Province, northwestern Argentina. The specimens resemble the type species of the genus, R. bronni, indicating a Pragian (Early Devonian) age for the strata, and suggesting the occurrence at this time of faunal exchange between the Old World Realm, particularly the Bohemian area, and the Malvinokaffric Realm. The taxon represents the first Early Devonian macrofaunal element in the Malvinokaffric Realm with global biostratigraphical significance.
6
Myrow, P. M., N. C. Hughes, and N. R. McKenzie. "Reconstructing the Himalayan margin prior to collision with Asia: Proterozoic and lower Paleozoic geology and its implications for Cenozoic tectonics." Geological Society, London, Special Publications 483, no. 1 (November 21, 2018): 39–64. http://dx.doi.org/10.1144/sp483.10.
Full textAbstract:
AbstractReconstructing the stratigraphic architecture of deposits prior to Cenozoic Himalayan uplift is critical for unravelling the structural, metamorphic, depositional and erosional history of the orogen. The nature and distribution of Proterozoic and lower Paleozoic strata have helped elucidate the relationship between lithotectonic zones, as well as the geometries of major bounding faults. Stratigraphic and geochronological work has revealed a uniform and widespread pattern of Paleoproterozoic strata >1.6 Ga that are unconformably overlain by <1.1 Ga rocks. The overlying Neoproterozoic strata record marine sedimentation, including a Cryogenian diamictite, a well-developed carbonate platform succession and condensed fossiliferous Precambrian–Cambrian boundary strata. Palaeontological study of Cambrian units permits correlation from the Indian craton through three Himalayan lithotectonic zones to a precision of within a few million years. Detailed sedimentological and stratigraphic analysis shows the differentiation of a proximal realm of relatively condensed, nearshore, evaporite-rich units to the south and a distal realm of thick, deltaic deposits to the north. Thus, Neoproterozoic and Cambrian strata blanketed the northern Indian craton with an extensive, northward-deepening, succession. Today, these rocks are absent from parts of the inner Lesser Himalaya, and the uplift and erosion of these proximal facies explains a marked change in global seawater isotopic chemistry at 16 Ma.
7
Nieto Sánchez, José Antolín. "Los más temibles por su indocilidad”: sobre la conflictividad artesana en la Edad Moderna española." Sociología del Trabajo, no. 98 (July 1, 2021): 1–12. http://dx.doi.org/10.5209/stra.77115.
Full textAbstract:
Este artículo estudia las diferencias del conflicto laboral español en la Edad Moderna atendiendo a dos de sus sistemas de organización manufacturera: las grandes concentraciones industriales (Reales Fábricas, arsenales, minas) y los pequeños talleres artesanos. En este estudio se analizan los protagonistas del conflicto, las causas que llevaron a la protesta, la organización de esta, los diferentes tipos de conflicto y la actitud de los directores de Reales Fábricas y maestros artesanos ante el conflicto suscitado por sus subalternos.
8
Ciairano, Silvia, Davide Marengo, Michele Settanni, and Giulio Vidotto. "Profili di personalità e rischio stradale in adolescenza: uno studio longitudinale in ambiente simulato e reale." RICERCHE DI PSICOLOGIA, no. 1 (April 2013): 33–61. http://dx.doi.org/10.3280/rip2012-001003.
Full text
9
Oliver, William A., James E. Sorauf, and Carlton E. Brett. "A unique occurrence of Endophyllum (rugose coral; Devonian) in eastern North America: An ecological and biogeographical puzzle." Journal of Paleontology 70, no. 1 (January 1996): 46–56. http://dx.doi.org/10.1017/s002233600002309x.
Full textAbstract:
Endophyllum is described for the first time from North America. The occurrence of a single, large colony in Middle Devonian strata in New York is both biogeographically and environmentally anomalous: it belongs to an Old World Realm genus but was found in the Eastern Americas Realm, and it occurred in a gray, ambocoeliid-bearing mudstone, a facies in which morphologically complex corals are otherwise unknown. Available evidence suggests that the coral lived not far from where it was found, possibly on a hardground or bank a few km north of the outcrop. Endophyllum ciurcai new species is described.
10
Blodgett, Robert B., and David M. Rohr. "Two new Devonian spine-bearing pleurotomariacean gastropod genera from Alaska." Journal of Paleontology 63, no. 1 (January 1989): 47–52. http://dx.doi.org/10.1017/s0022336000040944.
Full textAbstract:
Two new spine-bearing gastropods, Chlupacispira spinosa n. gen. and sp. and Spinulrichospira cheeneetnukensis n. gen. and sp., are described from the late Early Devonian (Emsian) and early Middle Devonian (Eifelian), respectively, of west-central Alaska. These represent the earliest reported spiny pleurotomariacean gastropods. Otherwise, spinose pleurotomariaceans are known from strata no older than Carboniferous age. Spinulrichospira cheeneetnukensis n. gen. and sp. appears to represent a more highly ornamented derivative of Ulrichospira Donald. Both new genera are part of the more highly ornamented fauna which occurred in warm equatorial waters of the Old World Realm during the Early and Middle Devonian, in contrast to more weakly ornamented shells of the Eastern Americas Realm and even more weakly ornamented (almost totally “plain”) shells of the Malvinokaffric Realm. The latter two realms are thought to represent subtropical to warm temperate and cool temperate to cool polar conditions, respectively.
11
Schlagintweit, Felix, and Mohsen Yazdi-Moghadam. "Moncharmontia De Castro 1967, benthic foraminifera from the middle-upper Cenomanian of the Sarvak Formation of SW Iran (Zagros Zone): a CTB survivor taxon." Micropaleontology 67, no. 1 (2021): 19–29. http://dx.doi.org/10.47894/mpal.67.1.03.
Full textAbstract:
Moncharmontia apenninca (De Castro 1966) is widely reported in the Upper Cretaceous (Turonian-Campanian) shallow-water successions of the Neotethyan realm (e.g., Italy, Croatia). With its "First Appearance Datum" (FAD) in the lowermost Turonian, it is considered a newcomer taxon in the aftermath of the Cenomanian/Turonian boundary (CTB) extinction event, and therefore a member of the Upper Cretaceous Global Community Maturation Cycle. Its common presence in the middle-pro parte upper Cenomanian Sarvak Formation and time-equivalent strata in Mexico (Valles-San Luis Potosi Platform) document that it represents a CTB extinction survivor taxon like Dicyclina, Nezzazata, Reticulinella and several others. The different local "FAD's" of Moncharmontia might possibly be linked to latitudinal differences, i.e., an earlier evolution of the species in the near-equatorial area (Mexico, Iran) compared to the low-middle latitudinal occurrences in the peri-Mediterranean realm (e.g., Italy, Turkey).
12
Fastovsky, David E. "Dinosaurs in Space and Time: The Geological Setting." Short Courses in Paleontology 2 (1989): 22–33. http://dx.doi.org/10.1017/s2475263000000829.
Full textAbstract:
The title of this chapter makes a promise that cannot be kept: that somehow there could be summarized in its few pages all the paleoenvironments of dinosaur-bearing strata through time. Dinosaurs were –as far as can be determined – ubiquitious in the terrestrial realm. It would be impossible to summarize the Recent terrestrial settings of birds (avian dinosaurs), let alone 135 million years of terrestrial settings. For this reason, this paper will be restricted to generalizations about ancient environments, highlighting particularly interesting or productive dinosaur-bearing localities in North America.
13
Luis García, Katia, Vivian Beatriz Elena Parnás, Kristof Maes, and Geert Lombaert. "Full scale measurements of a self-supporting tower using accelerometers and strain gauges." Ingeniería y Desarrollo 38, no. 1 (January 21, 2021): 259–78. http://dx.doi.org/10.14482/inde.38.1.531.38.
Full text
14
Cichowolski, Marcela, and Juan J. Rustán. "First report of Devonian bactritids (Cephalopoda) from South America: paleobiogeographic and biostratigraphic implications." Journal of Paleontology 91, no. 3 (April 26, 2017): 417–33. http://dx.doi.org/10.1017/jpa.2017.17.
Full textAbstract:
AbstractDevonian bactritids are described for the first time from South America. They come from siliciclastic rocks of the Talacasto Formation in the Precordillera Basin, west-central Argentina. The host strata span the Lochkovian–Emsian and contain other non-ammonoid cephalopods as well, thus refuting the alleged virtual absence of cephalopods in circumpolar Devonian basins from southwestern Gondwana (the Malvinokaffric Realm). We reportBactrites gracilisandDevonobactrites? sp., whose wide distribution contrasts with the endemic paleobiogeographic signature of some other taxonomic groups in these basins. Furthermore, new Lochkovian and Pragian records ofBactritessp. provide new insights into the earliest bactritid records worldwide.
15
Rosso, Marta. "La costellazione del ‘new Italian weird’ tra letteratura estrema e ipermodernità." ENTHYMEMA, no. 28 (January 1, 2022): 204–30. http://dx.doi.org/10.54103/2037-2426/14409.
Full textAbstract:
Il contributo ricostruisce la costellazione della narrativa italiana contemporanea più ‘strana’, soprannominata ‘new Italian weird’ nel dibattito on line che ha accompagnato il fenomeno editoriale tra il 2016 e il 2018, e la raffronta con i suoi corrispettivi negli Stati Uniti e in Europa per ragionare su come e perché i sistemi letterari si trasformano nel tempo. Una lettura semiologica e polisistemica ha permesso di ricondurre le modalità di questo recente sentire letterario a una più ampia condizione della contemporaneità, il cui carattere esasperato è stato definito anche in termini di ipermodernità e che oggi sembrerebbe implicare una sempre maggiore ibridazione tra i generi del romanzo. A caratterizzare questa nuova forma di letteratura, a suo modo estrema, è il ricorso al ‘weird’, qui inteso non come genere a sé ma come dispositivo ‘obliquo’, impiegato per aprire nuove prospettive e per oltrepassare gli stretti confini e le limitate possibilità di senso del reale.
16
Montgomery, Scott. "The Eye and the Rock: Art, Observation and the Naturalistic Drawing of Earth Strata." Earth Sciences History 15, no. 1 (January 1, 1996): 3–24. http://dx.doi.org/10.17704/eshi.15.1.9373301405572mr3.
Full textAbstract:
The first naturalistic drawings of geologic phenomena, particularly rock formations, are assumed by historians to have occurred early in the 19th century, when geology matured as a science. No less than three centuries earlier, however, the Netherlandish master, Jan Van Eyck, drew exposures of natural rock whose features are so remarkably accurate as to permit modern-day geologic analysis of their lithology, fossil content, sedimentary structures, and depositional environment. Van Eyck clearly studied, drew, and painted a specific outcrop "in the field," long before such practice had become common in art or science. As the first modern geologic "observer," Van Eyck greatly extended an existing tradition of naturalism with regard to organic phenomena (esp. plants, insects, human figures) fully into the realm of inorganic reality. In this, he far surpassed other scholar-artists, such as Leonardo da Vinci, who have been credited with similar achievements. Van Eyck's achievement proved exceptional. It was matched neither by later artists, scientists, or illustrators until the late 18th-early 19th century, when conventions in travel literature and landscape inspired new attention to the drawing of rock materials. The reasons for this historical gap have everything to do with the limitations of observation in early geological study, which show important parallels to those in art.
17
R, Saranya, and Anandakrishnan N. "Quantum Particle Swarm Optimization (QPSO) based Robust Estimation in Real-Time Ultrasound Strain Imaging." SIJ Transactions on Computer Science Engineering & its Applications (CSEA) 07, no. 02 (April 3, 2019): 01–10. http://dx.doi.org/10.9756/sijcsea/v7i2/06050150101.
Full text
18
Koch, William F. "Atlanticocoelia, new leptocoeliid (Brachiopoda) genus from the Devonian of eastern North America." Journal of Paleontology 70, no. 6 (November 1996): 1088–90. http://dx.doi.org/10.1017/s0022336000038786.
Full textAbstract:
Various workers have assigned Atrypa acutiplicata Conrad, 1841, to a number of leptocoeliid genera. Restudy of specimens previously examined by Boucot and Rehmer (1977) as part of a study of the community paleoecology of brachiopods of the Emsian and Eifelian strata of eastern North America has shown that A. acutiplicata does not belong to any existing genus of leptocoeliid. Therefore, the new genus Atlanticocoelia is proposed, with A. acutiplicata as the type species, for leptocoeliid brachiopods with a small, knoblike cardinal process, a brachial valve of moderate convexity, a broad sulcus, strong plications, subparallel dorsal adductor scars, and cordate pedicle diductor scars. Atlanticocoelia occurs in benthic assemblage 4 to 5 communities of the Emsian through Eifelian Appohimchi Province of the Eastern Americas Realm.
19
Ng, Kwok-Choi, and Brian Jones. "Sedimentology and diagenesis of Upper Mississippian to Lower Permian strata, Talbot Lake area, Jasper National Park, Alberta." Canadian Journal of Earth Sciences 26, no. 2 (February 1, 1989): 275–95. http://dx.doi.org/10.1139/e89-023.
Full textAbstract:
In the Talbot Lake area, the Upper Mississippian carbonate sequence comprises, in ascending order, the Turner Valley and Mount Head formations. The Mount Head Formation is informally divided into lower and upper members. The rocks of the Upper Mississippian originated by sedimentation associated with successive shallowing-upward sequences. On the basis of the fossils, lithologies, textural characters, and sedimentary structures, the Turner Valley Formation apparently resulted from sedimentation on open marine shoals and in a lagoon, the lower member of the Mount Head Formation from sedimentation in shallow subtidal to lower supratidal environments, and the upper member of the Mount Head Formation from deposition in upper intertidal to supratidal environments.The paraconformity between the lower and upper members of the Mount Head Formation records a short erosional break. A disconformity between the Upper Mississippian carbonates and the Upper Permian Ishbel Group displays paleotopographic relief and paleokarstic features developed during exposure in post-Mississippian times. The disconformity is overlain by a condensed sequence of Pennsylvanian to Permian strata.Major diagenetic modifications of the Upper Mississippian strata include dolomitization, silica replacement and cementation, carbonate cementation, and dedolomitization. A diagenetic realm comprising sea water, fresh water, and hypersaline brine was probably responsible for some of the complex diagenesis in these rocks.
20
Pyle, Leanne J., and Christopher R. Barnes. "Conodonts from the Kechika Formation and Road River Group (Lower to Upper Ordovician) of the Cassiar Terrane, northern British Columbia." Canadian Journal of Earth Sciences 38, no. 10 (October 1, 2001): 1387–401. http://dx.doi.org/10.1139/e01-033.
Full textAbstract:
This study examines the lower Paleozoic stratigraphy of the Cassiar Terrane from three key sections comprising an east-west transect across the terrane. The Cassiar Terrane, west of the Northern Rocky Mountain Trench, consists of a Neoproterozoic to Triassic succession and is a fragment of the Cordilleran Miogeocline that has been displaced northward. The amount of displacement from its original position remains controversial. Conodonts from the Cassiar Terrane have been previously reported from only a few reconnaissance studies. More than 3000 m of strata have been measured and examined in detail and 85 conodont samples collected. A total of 926 identifiable conodont elements are assigned to 31 species representing 21 genera. The conodonts are mainly representative of the Midcontinent Faunal Realm, but some also represent the Atlantic Realm. Conodonts from the upper Kechika Formation and base of the Road River Group are Early Ordovician (Tremadocian) in age, and those from the upper Road River Group range into the Upper Ordovician (Caradocian). The detailed Ordovician stratigraphy and temporal constraints established by conodont biostratigraphy provide for correlation to coeval facies of ancestral North America. The onset of Road River sedimentation in the mid-Tremadocian is, however, older than that in the Macdonald Platform to the east (early Arenigian). This onset timing may help link the Cassiar Terrane to a specific part of the miogeocline from which it was transported.
21
Pyle, Leanne J., Christopher R. Barnes, and Lee McKenzie McAnally. "Conodont biostratigraphy of the latest Cambrian - Early Ordovician upper McKay Group, southeastern British Columbia." Canadian Journal of Earth Sciences 44, no. 12 (December 1, 2007): 1713–40. http://dx.doi.org/10.1139/e07-047.
Full textAbstract:
The age of the upper McKay Group based on conodont biostratigraphy is latest Cambrian (Cordylodus proavus Zone) to late Early Ordovician (middle Floian; Oepikodus communis Zone). A collection of 12 940 conodont elements was recovered from 306 samples of upper McKay Group strata exposed in the Western Main Ranges of the southern Canadian Rocky Mountains, southeastern British Columbia. The conodont fauna is assigned to 53 species representing 30 genera. Twelve zones are recognized, two of which are cosmopolitan: Cordylodus proavus Zone and Iapetognathus Zone. Seven Midcontinent Realm zones, in ascending order, include Polycostatus falsioneotensis, Rossodus tenuis, Rossodus manitouensis, low diversity interval, Scolopodus subrex, and Acodus kechikaensis zones, and Tropodus sweeti Subzone (of the Oepikodus communis Zone). Three Atlantic Realm zones, in ascending order, include Cordylodus angulatus, Acodus deltatus, and Paroistodus proteus zones. The zonation for the upper McKay Group establishes correlation with the Survey Peak Formation and lower Outram Formation of the Bow Platform, and with the Kechika Formation and lower Skoki Formation of the Macdonald Platform and Kechika Trough in the northern Rocky Mountains. The McKay Group represents deposition during post-rift thermal subsidence of the margin, although its thickness, abrupt transition to black shale of the overlying Glenogle Formation, and intercalation of volcanogenic rocks imply a history of differential subsidence similar to that of the northern Cordillera, probably related to periodic extension.
22
Vozárová, Anna, Miloš Šmelko, Ilya Paderin, and Alexander Larionov. "Permian volcanics in the Northern Gemericum and Bôrka Nappe system: U-Pb zircon dating and the implications for geodynamic evolution (Western Carpathians, Slovakia)." Geologica Carpathica 63, no. 3 (June 1, 2012): 191–200. http://dx.doi.org/10.2478/v10096-012-0016-4.
Full textAbstract:
Permian volcanics in the Northern Gemericum and Bôrka Nappe system: U-Pb zircon dating and the implications for geodynamic evolution (Western Carpathians, Slovakia)U-Pb dating (SHRIMP) of magmatic zircon ages from the Northern Gemericum Permian volcanics (Petrová Hora Formation) yielded the Concordia age of 272.4 ± 7.3 Ma for basaltic andesite, as well as the Concordia age of 275.2 ± 4 Ma for rhyodacites. Both zircon ages correspond to the Cisuralian Epoch in the time span of the Kungurian Stage. Acquired206Pb/238U zircon age data support the nearly contemporaneous origin of the acid and basic volcanogenic members in the Northern Gemericum Permian strata. The bimodal volcanic suite proves the transtension/extension tectonic regime in the North Gemeric sedimentary basin during the Late Cisuralian. The magmatic zircon ages of rhyodacites, occurring in the lower thrust sheet of the Bôrka Nappe (Jasov Formation), gave a younger Concordia age of 266 ± 1.8 Ma proving the Guadalupian Epoch, in the time span of the Wordian/Capitanian. In comparison to the Northern Gemericum realm, this age refers to the relatively younger stage of rift-related extensional movements. In the wide Alpine-Dinarides realm the Middle Permian (Guadalupian) movements are related to the beginning of the Alpine sedimentary cycle. Thus, the Middle Permian rifting expresses the beginning of the formation of the future Meliata oceanic trough.
23
Ghanem, Hussam, Mikhail Mouty, and Jochen Kuss. "Biostratigraphy and carbon-isotope stratigraphy of the uppermost Aptian to Upper Cenomanian strata of the South Palmyrides, Syria." GeoArabia 17, no. 2 (April 1, 2012): 155–84. http://dx.doi.org/10.2113/geoarabia1702155.
Full textAbstract:
ABSTRACT Biostratigraphic and carbon-isotope data were used to introduce a high-resolution stratigraphic reference section of the Upper Aptian to Upper Cenomanian platform carbonates of the South Palmyrides in Syria. We studied the biostratigraphic evolution of the Zbeideh to Abou-Zounnar formations in two sections, based on 42 species of benthonic foraminifera and 38 species of planktonic foraminifera. Comparisons with other Tethyan assemblages allowed determining 11 biozones; six are based on planktonic foraminifera, and five on benthonic foraminifera. Four hiatuses (earliest Albian, Middle–Late Albian, Late Albian–Early Cenomanian, and Mid Cenomanian) are marked by hardgrounds or dolomitic intervals. The planktonic biozones Ticinella bejaouaensis, T. primula, T. praeticinensis, Rotalipora subticinensis, R. globotruncanoides and R. cushmani co-occur with the following benthonic biozones: Mesorbitolina texana partial range zone, M. subconcava range zone, Neoiraqia convexa taxon-range zone, Praealveolina iberica interval zone and Pseudedomia drorimensis range zone. Within this biostratigraphic framework, a new carbon-isotope curve from the South Palmyrides was compared with δ13C records of the Tethyan Realm and England that allows identifying several biotic events and Oceanic Anoxic Events (OAE), recorded in the Upper Albian to Upper Cenomanian succession. The combination of sequence-stratigraphic interpretations and comparisons, with our results have led to an improved understanding of the Cretaceous platform architecture of the South Palmyrides that links the Arabian Platform to the east with the Levant Platform to the southwest.
24
Dines, Nick. "What’s in a word? Contextual diversity, urban ethnography and the linguistic limits of the street." Sociological Review 66, no. 5 (April 17, 2018): 952–67. http://dx.doi.org/10.1177/0038026118771289.
Full textAbstract:
This article takes to task a common assumption within Anglophone scholarship that conceives the street as a preeminent site of urban life, arguing that this sociological truism has worked to obscure the role of other spaces, terms and experiences across different historical, geographical and linguistic contexts. In response, and building on recent reappraisals in sociology of the work of Raymond Williams, the aim of this article is to analyse the street as a particular keyword and reflect on how a cultural materialist approach to lexical change can be incorporated into the practices of urban ethnography and translation. To develop its methodological argument, the article draws on the author’s research on Italian cities, where rather than the strada (street), the piazza and the vicolo (alleyway) have typically commanded a more prominent place in ideas about the public realm. At the same time, the disparate meanings of these two spatial forms attest to the uneven and disputed positions of different Italian cities within national urban culture. In conclusion, the article argues for greater attention to be paid to variations in language use vis-a-vis urban spatial forms as the prerequisite for a more incisive sociology of the street.
25
Schulz, Bo Pagh, Madeleine Larissa Vickers, Jennifer Huggett, Henrik Madsen, Claus Heilmann-Clausen, Henrik Friis, and Erwin Suess. "Palaeogene glendonites from Denmark." Bulletin of the Geological Society of Denmark 68 (April 1, 2020): 23–35. http://dx.doi.org/10.37570/bgsd-2020-68-03.
Full textAbstract:
Pristinely preserved mineral pseudomorphs called glendonites, up to 1.6 m long, from the Palaeogene strata of Denmark allow detailed crystallographic characterisation and add to the understanding of the transformation of the precursor mineral, ikaite (CaCO3·6H2O), to calcite, which constitutes the glendonite. We describe Danish pseudomorphs after ikaite from two localities and formations: the Early Eocene Fur Formation and the Late Oligocene Brejning Formation. This detailed study highlights that key aspects such as morphology and mode of occurrence of these ancient glendonites are identical to those of their parent mineral ikaite, when it grows in marine sediments. Systematic distortion of the angles in glendonite and marine sedimentary ikaite relative to the ideal ikaite symmetry may arise due to the incorporation of organic matter into the crystal structure, and we demonstrate the similarity between modern and ancient ikaite formation zones in the marine sedimentary realm with respect to organic matter.
26
Schultz, Bo Pagh, Madeleine L. Vickers, Jennifer Huggett, Henrik Madsen, Claus Heilmann-Clausen, Henrik Friis, and Erwin Suess. "Palaeogene glendonites from Denmark." Bulletin of the Geological Society of Denmark 68 (March 29, 2022): 23–35. http://dx.doi.org/10.37570/bgsd-2020-68-03-rev.
Full textAbstract:
Pristinely preserved mineral pseudomorphs called glendonites, up to 1.6 m long, from the Palaeogene strata of Denmark allow detailed crystallographic characterisation and add to the understanding of the transformation of the precursor mineral, ikaite (CaCO3·6H2O), to calcite, which constitutes the glendonite. We describe Danish pseudomorphs after ikaite from two localities and formations: the Early Eocene Fur Formation and the Late Oligocene Brejning Formation. This detailed study highlights that key aspects such as morphology and mode of occurrence of these ancient glendonites are identical to those of their parent mineral ikaite, when it grows in marine sediments. Systematic distortion of the angles in glendonite and marine sedimentary ikaite relative to the ideal ikaite symmetry may arise due to the incorporation of organic matter into the crystal structure, and we demonstrate the similarity between modern and ancient ikaite formation zones in the marine sedimentary realm with respect to organic matter.
27
OKUYUCU, CENGİZ. "Biostratigraphy and systematics of late Asselian–early Sakmarian (Early Permian) fusulinids (Foraminifera) from southern Turkey." Geological Magazine 145, no. 3 (February 19, 2008): 413–34. http://dx.doi.org/10.1017/s0016756808004482.
Full textAbstract:
AbstractThe Anatolian Platform, which was a part of the Gondwanan Platform, is mainly characterized by carbonate-dominated deposits ranging in age from Devonian to Permian. The biostratigraphy and systematics of a late Asselian–early Sakmarian fusulinid fauna from the Anatolian Platform including Eastern and Central Taurides have been investigated in three sections: Özbek Hill, Eskibey and Bademli. Twenty-four fusulinid taxa, belonging to twelve genera, were determined in a single fusulinid zone dated as late Asselian–early Sakmarian. Early–middle Asselian fusulinid faunas have not been observed in any of the measured sections throughout the Anatolian Platform. This indicates that lower to middle Asselian deposits are represented by an interval characterized by quartz sandstone overlying upper Gzhelian strata. Five new species (Pseudochusenella anatoliana, Pseudofusulinoides altineri, Pseudofusulinoides convexus, Pseudofusulinoides subglobosus and Pseudofusulinoides vachardi) are described in this study. The Early Permian fusulinid fauna correlates very well with the fauna of other sections in the Palaeotethyan realm (Southern Alps, Central Asia, Southern China and Japan).
28
Blodgett, Robert B., Jiří Frýda, and Alfred C. Lenz. "Semitubina yukonensis new species, first occurrence of this biogeographically distinctive Old World Realm gastropod genus in the Lower Devonian of the western hemisphere." Journal of Paleontology 75, no. 2 (March 2001): 466–70. http://dx.doi.org/10.1017/s0022336000018266.
Full textAbstract:
Despite the rapidly expanding knowledge of Lower Devonian brachiopod faunas of the Western Cordillera of Canada (Lenz, 1976, 1977a, 1977b, 1982; Ludvigsen, 1970; Perry, 1984; Perry and Lenz, 1978; Perry et al., 1974, 1981), equivalent data on coeval gastropod faunas from this region are non-existent; to date, no publications have appeared in which gastropods have been described. Blodgett et al. (1988, table 1) provided faunal lists for two Lower Devonian localities in Western Canada: 1) Lochkovian-Emsian age collections from the Mackenzie Mountains, Northwest Territories, collected by the late D. G. Perry as part of his Ph.D. dissertation (Perry, 1984); and 2) an early Emsian collection from the Mt. Lloyd George area, British Columbia. We are currently examining the gastropod material recovered by A. C. Lenz from his richly diverse collections in the Royal Creek area, Yukon Territory, equivalent in age to those gathered by D. G. Perry from the Mackenzie Mountains. This note is the first of several papers focused on these paleobiogeographically significant faunas, and it is our desire to ultimately make clear the character of this Early Devonian province, which appears to include strata of British Columbia, Yukon and Northwest Territories, as well as the non-accreted portion of adjacent east-central Alaska.
29
Stefanati, Michele Ronchi. "Per una linea leopardiana dell’impegno: Sulla matrice etico-politica dell’opera di Gianni Celati degli anni Duemila." Quaderni d'italianistica 39, no. 1 (May 9, 2019): 51–80. http://dx.doi.org/10.33137/q.i..v39i1.32633.
Full textAbstract:
Per lungo tempo, una certa tendenza critica è stata solita legare il concetto di impegno a quello di realismo, indicando come “letteratura dell’impegno” soltanto le scritture di rappresentazione e denuncia di una realtà sociale o politica e contrapponendola rigidamente al postmodernismo, visto come sinonimo di disimpegno. All’alba degli anni Duemila, nuovi studi hanno aperto strade diverse, cogliendo la complessità del concetto di impegno nelle sue numerose trasformazioni, individuandone linee di tendenza e momenti di rottura nel corso del Novecento, ma affermando la persistenza di motivi di critica etica e sociale anche in anni solitamente considerati di totale disimpegno e introversione. L’opera di Gianni Celati rappresenta un esempio di impegno, mai dichiarato, a cui non corrisponde nessun “ritorno al reale”, anzi in aperto contrasto rispetto ad esso. Quello di Celati è un “impegno fantasticante”, laddove l’intera sua opera, dagli esordi negli anni 1970 fino agli ultimi scritti, sembra partire da una considerazione critica sulla società contemporanea, sviluppando tendenze anti-autoritarie, anti-gerarchiche, anti-consumistiche e anti-egemoniche espresse, però, senza alcun ricorso al realismo. Il presente studio si concentra sulle forme di impegno etico-politico nell’opera di Celati degli anni Duemila, anni che hanno dato vita, attraverso la collaborazione alla rivista Zibaldoni e altre meraviglie, a quella che si potrebbe chiamare una “linea leopardiana dell’impegno”, per i numerosi riferimenti all’opera di Leopardi e al ruolo che essa ha avuto in quest’ottica.
30
Wagreich, M. ""OAE 3" – regional Atlantic organic carbon burial during the Coniacian–Santonian." Climate of the Past 8, no. 5 (September 20, 2012): 1447–55. http://dx.doi.org/10.5194/cp-8-1447-2012.
Full textAbstract:
Abstract. The Coniacian–Santonian time interval is the inferred time of oceanic anoxic event 3 (OAE 3), the last of the Cretaceous OAEs. A detailed look on the temporal and spatial distribution of organic-rich deposits attributed to OAE 3 suggests that black shale occurrences are restricted to the equatorial to mid-latitudinal Atlantic and adjacent basins, shelves and epicontinental seas like parts of the Caribbean, the Maracaibo Basin and the Western Interior Basin, and are largely absent in the Tethys, the North Atlantic, the southern South Atlantic, and the Pacific. Here, oxic bottom waters prevailed as indicated by the widespread occurrence of red deep-marine CORBs (Cretaceous Oceanic Red Beds). Widespread CORB sedimentation started during the Turonian after Oceanic Anoxic Event 2 (OAE 2) except in the Atlantic realm where organic-rich strata continue up to the Santonian. The temporal distribution of black shales attributed to OAE 3 indicates that organic-rich strata do not define a single and distinct short-time event, but are distributed over a longer time span and occur in different basins during different times. This suggests intermittent and regional anoxic conditions from the Coniacian to the Santonian. A comparison of time-correlated high-resolution δ13C curves for this interval indicates several minor positive excursions of up to 0.5‰, probably as a result of massive organic carbon burial cycles in the Atlantic. Regional wind-induced upwelling and restricted deep basins may have contributed to the development of anoxia during a time interval of widespread oxic conditions, thus highlighting the regional character of inferred OAE 3 as regional Atlantic event(s).
31
Wagreich, M. ""OAE 3" – a low- to mid-latitude Atlantic oceanic event during the Coniacian-Santonian." Climate of the Past Discussions 8, no. 2 (April 16, 2012): 1209–27. http://dx.doi.org/10.5194/cpd-8-1209-2012.
Full textAbstract:
Abstract. The Coniacian-Santonian time interval is the inferred time of oceanic anoxic event 3 (OAE 3), the last of the Cretaceous OAEs. A detailed look on the temporal and spatial distribution of organic-rich deposits attributed to OAE 3 suggests that black shale occurrences are restricted to the equatorial to mid-latitudinal Atlantic and adjacent basins, shelves and epicontinental seas like parts of the Caribbean, the Maracaibo Basin and the Western Interior Basin, and are largely absent in the Tethys, the North Atlantic, the southern South Atlantic, and the Pacific. Here, oxic bottom waters prevailed as indicated by the widespread occurrence of red deep-marine CORBs (Cretaceous Oceanic Red Beds). Widespread CORB sedimentation started during the Turonian after Oceanic Anoxic Event 2 (OAE 2) except in the Atlantic realm where organic-rich strata continue up to the Santonian. The temporal distribution of black shales attributed to OAE 3 indicates that organic-rich strata do not define a single and distinct short-time event, but are distributed over a longer time span and occur in different basins during different times. This suggests intermittent and regional anoxic conditions from the Coniacian to the Santonian. A comparison of time-correlated high-resolution δ13C curves for this interval indicates several minor positive excursions of about 0.5 permil, probably as a result of massive organic carbon burial cycles in the Atlantic. Regional wind-induced upwelling and silled deep basins may have contributed to the development of anoxia during a global oxic time interval, thus highlighting the regional character of inferred OAE 3 as an Atlantic anoxic event (AAE).
32
Goenner, Hubert. "The Reaction to Relativity Theory I: The Anti-Einstein Campaign in Germany in 1920." Science in Context 6, no. 1 (1993): 107–33. http://dx.doi.org/10.1017/s0269889700001332.
Full textAbstract:
The ArgumentDevelopments in theoretical physics, even when they are revolutionary for physics, usually donotenter public awareness. The reaction to the special relativity theory is one of the few exceptions. The conceptual changes brought by special relativity to our notions of space and time, induced a lively debate not only within intellectual circles but in many strata of the educated middle class. In this article, I focus on a particular moment of public reaction to special and general relativity theory and to its creator Albert Einstein. I try to paint a picture of the anti-Einstein campaign in Germany of 1920, with finer brush strokes than those applied previously by others. My aim is to embed the campaign into the cultural and political climate of the Weimar republic. Without leaving the realm of physics only a superficial understanding of what happened seems possible. My thesis is that the anti-Einstein-campaign was organized, and the physicists involved in it (ab)used, mainly in order to rally support for one of the German right-wing parties, the Deutschnationale Volkspartei.
33
Di Pietro, Maria Luisa, and Maria Beatrice Fisso. "Donna e lavoro: considerazioni etico-giuridiche sulla prevenzione del rischio riproduttivo." Medicina e Morale 44, no. 3 (June 30, 1995): 447–87. http://dx.doi.org/10.4081/mem.1995.980.
Full textAbstract:
E' oramai noto che le attività lavorative possono influenzare, in modo diretto o indiretto, la salute: da questa consapevolezza ha avuto origine, nel tempo, una sempre maggiore attenzione nei confronti degli effetti nocivi di sostanze "sospette" in ambiente di lavoro. In questo articolo viene affrontato un aspetto particolare del rischio lavorativo, cioè il rischio a seguito dell'esposizione della donna a sostanze chimiche o ad agenti fisici o biologici che possono alterare la sua capacità riproduttiva o essere causa di gravi danni alla prole che è stata o verrà concepita. Dopo aver fatto distinzione tra rischio riproduttivo (la possibilità che una sostanza possa interferire con o impedire il concepimento) e rischio di sviluppo (la possibilità di produrre nel nascituro o successivamente nel nato fino alla pubertà anomalie strutturali, deficit funzionali o la morte), e aver analizzato il meccanismo di azione delle sostanze chimiche e degli agenti fisici e biologici più di frequente presenti in ambiente di lavoro, e precisato il momento di interferenza (la oogenesi, la gravidanza, l'allattamento), le Autrici individuano ed esaminano criticamente le possibili modalità di prevenzione del rischio riproduttivo e di sviluppo. Dall'individuazione delle situazioni a rischio alla messa a punto delle misure di controllo necessarie per ridurre o eliminare l'esposizione dei lavoratori, all'informazione dello stesso sull'esistenza e sull'entità del rischio: un'analisi che, in un'ottica personalistica, vorrebbe indicare - anche alla luce delle normative vigenti - nuove strade perché si possa attuare una reale tutela della lavoratrice e una vera politica di protezione fetale.
34
Seng, Anabela Fong Keng. "THREE MILLENNIA OF CHINESE POETRY." Revista Brasileira de Literatura Comparada 22, no. 41 (December 2020): 103–9. http://dx.doi.org/10.1590/2596-304x20202241afk.
Full textAbstract:
Abstract Poetry has a history of thousands of years in China and can be said to be the shining jewel in the crown of Chinese literature, occupying a major proportion in her history. Having originated from folk songs, the Chinese poetry has produced a large number of brilliant examples from the Western Zhou Dynasty (1046-771 BC) to the Chunqiu (Spring and Autumn) Period (770-476 BC). China has, since ancient times, maintained a tradition of education in poetry, which is used to educate the people and arouse their intelligence. Through the reading, studying and writing of poetry, it is possible to instruct and cultivate the character of young pupils, as well as to promote children’s creative thinking, logical dialectics and humanistic consciousness. In addition, reciting, learning and writing poetry has the ability to cultivate one’s temperament, allowing people of all social strata, professional occupation and age to cleanse and purify their minds. The realm of poetry has the same effect of calming the soul as religious belief. This article shows the highlights of three millennia of Chinese poetry to the readers or scholars whose native language is not Chinese.
35
Bizzarro, Martin, and Pierre J. Lespérance. "Systematics of some Lower and Middle Devonian spiriferid brachiopods from Gaspé with a revision of the superfamily Delthyridoidea." Journal of Paleontology 73, no. 6 (November 1999): 1056–77. http://dx.doi.org/10.1017/s0022336000030985.
Full textAbstract:
The component subfamilies of the Delthyridoidea are critically reviewed and subjected to phylogenetic analysis. This shows the presence of two clades, assigned to the Delthyrididae and Acrospiriferidae, within the superfamily. The subfamilial categories are redefined mainly on the basis of the characters used in the phylogenetic analysis. The spiriferid, mainly delthyridide, Gaspé fauna is formally revised and redescribed. This new taxonomic treatment leads to more precise biostratigraphy and to the recognition of a new subfamily, the Gaspespiriferinae, based on the new genus Gaspespirifer. Five new species are described: Howellella (Howellella) forillonensis, Brachyspirifer (Brachyspirifer) briseboisi, Paraspirifer desbiensi, Brevispirifer florentinus, and B. quebecensis, The occurrence of Brevispirifer species with Middle Devonian chonetaceans confirms the presence of marine Eifelian strata in the Matapédia Valley. Paraspirifer desbiensi n. sp. and two species left in open nomenclature, Vandercammenina sp. and Mucrospirifer sp., have considerable biostratigraphic and biogeographic significance in the Lower Devonian. The first occurrence in the Eastern Americas Realm of the typically Rhenish genera Brachyspirifer, Paraspirifer, and Vandercammenina are in Gaspé. This reinforces the hypothesis that Gaspé served as a stepping stone for Rhenish species invading North America in Pragian and Emsian times, as previously suggested by bivalve biogeography.
36
Costato, Luigi. "Regime disaccoppiato, Trattato di Lisbona e obiettivi della Pac verso il 2020." AGRICOLTURA ISTITUZIONI MERCATI, no. 2 (October 2011): 13–27. http://dx.doi.org/10.3280/aim2011-002002.
Full textAbstract:
Le regole del libero mercato e della concorrenza non riescono, in agricoltura, a produrre effetti positivi tali da compensarne gli svantaggi. D'altra parte è lo stesso art. 39 del Tfue, che riprende senza modifiche le disposizioni sull'agricoltura del vecchio Trattato CE, a stabilire che le regole della concorrenza possano non essere applicate al settore di produzione e commercio dei prodotti agricoli e a porre come obiettivi la sicurezza degli approvvigionamenti, adeguati redditi per gli agricoltori e prezzi ragionevoli ai consumatori. Eppure, nell'intraprendere la strada per l'ennesima riforma della Pac sembra che la Commissione intenda restare ben salda sulle posizioni che, a partire dalla riforma del 2003 e dall'introduzione del, hanno provocato il lungo periodo di difficoltà di reddito e di mercato al mondo agricolo. Sebbene, infatti, la Commissione si dimostri capace di individuare le reali sfide che l'agricoltura europea è chiamata ad affrontare, tuttavia non indica proposte coerenti con i predetti scopi, così come non vengono forniti significativi elementi di novità quando si affrontano argomenti specifici quali, ad esempio, i pagamenti diretti o le misure di mercato. Ciò che, però, risulta ancor meno confortante è il fatto che, tra le tre diverse attuazioni della riforma proposte, sembri prevalere quella volta a favorire un abbandono graduale delle misure di sostegno del reddito e della maggior parte delle misure di mercato quando, invece, sarebbe auspicabile tornare ad incentivare la produzione alimentare, garantendo, anche attraverso le scorte, la sicurezza degli approvvigionamenti.
37
Menges, Achim. "Performative morphology in architecture: Integrative design research by the Institute for computational design." SAJ - Serbian Architectural Journal 5, no. 2 (2013): 92–105. http://dx.doi.org/10.5937/saj1302092m.
Full textAbstract:
Computation, in its most basic meaning, refers to the processing of information. In this way, both machinic processes operating in the binary realm of the digital, as well as material processes operating in the complex domain of the physical can be considered computational. While there is a strong bias towards the former in contemporary design, sporadic investigations of the later have also occurred in architecture. What is more rarely explored, though, is the territory where machine computation and material computation potentially overlap, where they not simply co-exist but intensely interact in the design process. Such an integrative approach to machine and material computation forms a central part of the research pursued at the Institute for Computational Design at the University of Stuttgart. This paper will introduce the related design research through the presentation of three research projects. The first part of the paper focuses on the explanation of the theoretical framework of the Institute's approach to design computation, which finds its conceptual roots in the integrative processes of biological becoming rather than the striated processes of established technological production. It seeks to outline novel possibilities for a higher level of integration of form, information and performance in architecture through the possible synthesis of machine and material computation in morphogenetic design. The second part of the paper will provide specific examples of such a computational approach by introducing three related research areas. The possible integration of material behaviour as an active driver in computational design processes will be introduced through a first research project focusing on bending-active structures constructed from thin plywood lamellas. The second research project constitutes an example for the integration of materialization characteristics by encoding the possibilities and limits of robotic fabrication for modular wood shell structures in design computation. The third research project introduces the integration of material structure by embedding the complex reciprocities of form, material, structure and performance resulting from robotic carbon and glass fibre filament winding in a generative morphogenetic design process.
38
Nurgiyanti, Tanti, and Dwi Nur Laela Fithriya. "Peran Indonesia dalam Meningkatkan Daya Saing Produk Kosmetik di Pasar Asean Melalui E-Commerce." Nation State Journal of International Studies 2, no. 2 (December 31, 2019): 173–86. http://dx.doi.org/10.24076/nsjis.2019v2i2.165.
Full textAbstract:
Trade liberalization has been carried out through the ASEAN Economic Community (AEC). Barriers to trade both goods and services are no longer found. Through market trade liberalization, ASEAN countries are increasingly open to competition. E-Commerce trade is a trade that was born due to the development of information technology. Through trade E-Commerce creates opportunities and challenges for countries in Southeast Asia. One product that is widely traded is cosmetics. The cosmetics industry has a strategic opportunity to increase the income of Southeast Asian countries, especially Indonesia. Promising markets, abundant raw materials and the ability to absorb labor are quite a number of industries to be reckoned with. It is interesting to study further the existence of strata that sells cosmetic products both at home and abroad through E-Commerce trading continues to increase. But on the other hand local Indonesian cosmetic products are not able to compete with foreign products. As a result, losses can be experienced by cosmetic products SME entrepreneurs. This study is intended to determine the role of the Indonesian government in enhancing the competitiveness of cosmetic products in the Asean realm as well as regulations that regulate cosmetics trade through the use of e-commerce.
39
Nichols, Aidan. "John Henry Newman and the Illative Sense: A Re-consideration." Scottish Journal of Theology 38, no. 3 (August 1985): 347–68. http://dx.doi.org/10.1017/s0036930600041004.
Full textAbstract:
The aim of this article is to provide an historical description of an important piece of Victorian theology, and subsequently to suggest a new context, or rather a new content for a familiar theme. Firstly, it will consider in what sense Newman may be called a ‘natural theologian’; secondly, it will give an account of the notion of the illative sense within the developing pattern of Newman's thought; finally, it will suggest that, by a unilateral concentration on moral experience — the ‘voice of conscience’ — Newman failed to do justice to the full significance of his own argumentation. The point of the illative sense is not that it helps us to identify any one experiential content, or area of reflection, which might lead us to theistic belief, but that it provides an overall context in which a variety of experiential strata and argumentative strategies may be displayed. Newman was, perhaps, too dominated by an autobiographical sense in the realm of fundamental belief in God to identify and correct the individualism which in dogmatic theology proper he would have avoided. Our theistic materials do not lie simply within our own breasts, but in an inter-rogation, Gadamer-like, of the entire theistic tradition as that is mediated to us by the classic texts of our predecessors.
40
Trębacz, Ewa. "Depth Modulation: Composing motion in immersive audiovisual spaces." Organised Sound 17, no. 2 (July 19, 2012): 156–62. http://dx.doi.org/10.1017/s1355771812000088.
Full textAbstract:
The field of electroacoustic music has witnessed years of extensive exploration of aural spatial perception and an abundance of spatialisation techniques. Today the growing ubiquity of visual 3D technologies gives artists a similar opportunity in the realm of visual music. With the use of stereoscopic video we now have the ability to compose individual depth cues independently. The process of continuous change of the perceived depth of the audiovisual space over time is being referred to as depth modulation, and can only be fully appreciated through motion.What can be achieved through the separation and manipulation of visual and sonic spatial cues? What can we learn about the way we perceive space if the basic components building our understanding of the surrounding environment are artificially split and re-arranged?Visual music appears to be a perfect field for such experimentation. Strata of visual and aural depth cues can be used to create audiovisual counterpoints in three-dimensional spaces. The choice of abstract imagery and the lack of obvious narrative storylines allow us to focus our perception on the evolution of the immersive audiovisual space itself. A new language of an immersive audiovisual medium should emerge as a delicate, ever-changing balance between all previously separated and altered components.
41
Morton, Nicol, Vasily V. Mitta, and John R. Underhill. "Ammonite occurrences in North Sea cores: implications for Jurassic Arctic–Mediterranean marine seaway connectivity." Scottish Journal of Geology 56, no. 2 (August 14, 2020): 175–95. http://dx.doi.org/10.1144/sjg2019-030.
Full textAbstract:
The paucity of ammonite recovery from North Sea wells has meant that offshore correlations are largely dependent upon microfossil assemblages. While rare, ammonites have been found in a few boreholes during the course of oil exploration activities. The occurrence of ammonites in ten wells in the UK sector of the Viking Graben and the Moray Firth rift arms provides a new basis by which to demonstrate that there was a distinct separation between Arctic and sub-Mediterranean species that lasted from Bajocian to Early Callovian times. Five wells contain ‘Boreal Bathonian' ammonites from the Arctic Realm. Arctocephalites from the Boreal Arcticus Zone (uppermost Bajocian) correlates basinal partly anoxic mudstones in the Beryl Embayment (9/13b) with both bioturbated siltstones in the southern Viking Graben (9/10b), and calcareous mudstones in the East Shetland Basin (211/21). Upper Bajocian Pompeckji Zone Cranocephalites and younger Arcticoceras from Lower to Middle Bathonian Greenlandicus, Ishmae and Cranocephaloide zones are confined to 211/21 demonstrating that the marine transgression began earlier and lasted longer. A Cadoceras from well 3/3-8 dates to the Lower Callovian Koenigi and Calloviense zones during which renewed extensional faulting re-established ammonite migration routes between the Boreal and sub-Mediterranean realms. A Middle Oxfordian (Densiplicatum Zone) Perisphinctes from well 22/5b-8 confirms an episode of northward migration from the sub-Mediterranean into the Boreal Realm. Upper Oxfordian (Regulare to Rosenkantzi zones) Amoeboceras in wells 211/21-1 and 9/13b-19 are close to Upper Bajocian/Lower Bathonian faunas, suggesting an absence of Upper Bathonian to Middle Oxfordian strata as a result of rift-related footwall uplift and erosion. In four wells from Block 15/21 (-4, -11, -12A and -25) Lower Kimmeridgian ammonites have been documented, including Rasenia, Amoebites, Aulacostephanoides and Zenostephanoides, from the Baylei (?), Cymodoce, Mutabilis and Eudoxus zones, the latter (confirmed at well 13/28b-8) dating a widespread regional marine flooding surface in the Inner Moray Firth.Supplementary material: The detailed measurements of dimensions of the ammonites described are available at: https://doi.org/10.6084/m9.figshare.c.5087313
42
Mitchell, Charles, Edsel D. Brussa, and Jörg Maletz. "A mixed isograptid-didymograptid graptolite assemblage from the Middle Ordovician of west Gondwana (NW Bolivia): Implications for graptolite paleoecology." Journal of Paleontology 82, no. 6 (November 2008): 1114–26. http://dx.doi.org/10.1017/s0022336000055323.
Full textAbstract:
Black shales of the Coroico Formation are part of a thick succession of Lower and Middle Ordovician strata that were deposited in the Cordillera Oriental foreland basin along the margin of West Gondwana. The basin was inhabited primarily by a cool-water, Atlantic-type graptolite fauna. Newly discovered material from rocks that crop out near the town of Consata in NW Bolivia include unexpected warm-water or Pacific-type elements such as Parisograptus caduceus and Pseudotrigonograptus within an assemblage dominated by abundant pendent Didymograptus specimens, Cryptograptus schaeferi, and diplograptaceans such as Oelandograptus oelandicus and Hustedograptus bulmani n. sp. Parisograptus caduceus has generally been considered to be restricted to oceanic depths below those of the epipalagic realm that occupied continental shelves, whereas the remainder of the assemblage is more characteristic of relatively shallow water, epicratonic sites. We interpret this mixed assemblage to be the Atlantic Province, West Gondwanan equivalent of the off-shore isograptid biofacies that is much more widely known from low latitude sites around the globe. These results suggest that in this region of West Gondwana, the properties of local water masses (productivity and physical features such as temperature, salinity, or oxygenation) strongly influenced graptolite species distribution and led to biofacies differentiation among coeval assemblages. It also suggests that some isograptids inhabited the epipelagic biotope in mid to high latitude regions. The new species Hustedograptus bulmani is described herein.
43
Ramos, Amparo. "Transition from alluvial to coastal deposits (Permian–Triassic) on the Island of Mallorca, western Mediterranean." Geological Magazine 132, no. 4 (July 1995): 435–47. http://dx.doi.org/10.1017/s001675680002149x.
Full textAbstract:
AbstractNon-marine redbeds (Permian and Triassic) in the island of Mallorca consist of a 0.4 km-thick alluvial succession that passes upwards into siliciclastic–carbonate coastal deposits. Tectonics and sealevel changes have been the main influences in their evolution. Low in this succession (the ‘Areniscas y lutitas de Port des Canonge’ unit) sandstone sheets with lateral accretion surfaces (macroscale inclined strata) and mudstones with frequent exposure structures are interpreted as the products of a sinuous alluvial system and floodplain. Climatic fluctuations are considered to be responsible for some significant up-section changes in the evolution of the alluvial deposits. Low-angle or horizontally stratified sandy units, interpreted as the result of flash floods, alternate upwards with point-bar deposits in the ‘Areniscas de Asá’. The hydrological response to minor climatic changes was evidently nearly instantaneous due to the lack of significant vegetation cover.During accumulation of mudstones and sandstones of the overlying ‘Lutitas y Areniscas de Son Serralta’ unit, the interpreted environment of deposition changed from a distal braidplain, mainly constructed by superposition of sandy bedforms with straight or linguoid crestlines in low sinuosity river channels, into a coastal plain with evidence of both continental and marine influences. The overlying carbonate platform (Muschelkalk) marks the development of a more homogeneous marine environment resulting from the Tethyan transgressive event that affected the whole peri-Mediterranean realm during the Anisian (middle Triassic).
44
Repetski, J. E., M. E. Taylor, D. S. Collins, A. R. Palmer, G. D. Wood, and R. C. Tobin. "Integrating paleontology, geothermometry, and sedimentology in determining the history of the Reelfoot Basin, southern midcontinent, U.S.A." Paleontological Society Special Publications 6 (1992): 243. http://dx.doi.org/10.1017/s2475262200008030.
Full textAbstract:
The northeast-trending Reelfoot basin, extending from northeast Arkansas and westernmost Tennessee into southeastern Missouri, southernmost Illinois, and westernmost Kentucky, is geologically, and socioeconomically, significant because it is co-extensive with the New Madrid Seismic Zone, one of the most seismically active areas of the central and eastern United States. The basin has been periodically active from its inception as a rift basin in the Proterozoic to the present and has accumulated up to at least 5,000 m of sediment, including up to at least 1 km of Cretaceous and Tertiary sedimentary strata near the head of the Mississippi Embayment. Structural and stratigraphic interpretations within the subsurface pre-Mesozoic part of the basin have been based almost entirely on geophysical and physical stratigraphic criteria; these interpretations have been loosely constrained due to an extreme sparsity of drillhole data through the Paleozoic sequence. Recent analysis of Cambrian and Ordovician fossils (conodonts, palynomorphs, brachiopods, and trilobites) from cuttings and core from a very few drillholes allows establishment of the beginnings of a verifiable stratigraphy for this part of the sequence. The paleontological data also provide (1) biofacies evidence for interpretations of the depositional setting during part of the Late Cambrian and Early Ordovician interval and (2) thermal maturation data pertaining to the post-depositional geothermal history of these strata.Upper Cambrian phosphatic brachiopods and trilobites provide improved correlations between strata in the basin, the Ozark shelf to the northwest, and the Upper Mississippi River Valley. Cold-water-realm palynomorphs and trilobites from siliciclastic rocks of turbiditic origin in the central part of the Reelfoot basin support an interpretation, based on sedimentary structures in a short interval of core, of a deep-water basinal origin for these strata.Lower Ordovician conodonts provide a biostratigraphy for the carbonate rocks of this part of the sequence; correlations can be made with the shallow-water sequences of the Knox, Prairie du Chien, and Arbuckle Groups, and the Ozark sequence of the adjacent shelf areas to the east, north, and west. The uppermost Lower Ordovician strata in the basin record a short-term incursion of cooler water environments, reflected by the character of both the conodont fauna and the lithofacies. The youngest Paleozoic dates known from the basin south of the Pascola arch are latest Ibexian (Early Ordovician).Thermal alteration indices of both the Cambrian palynomorphs (organic-walled microphytoplankton) and Ordovician conodonts in the deeper parts of the basin, corroborated by fluid inclusion thermometry, vitrinite reflectance, and other geochemical techniques, are of higher values than predicted using any published estimates of overburden burial. These maturation values most likely reflect burial enhanced by the passage of hydrothermal fluids on a regional scale; they place constraints on interpretations of the tectonothermal evolution of the basin.
45
LESMES, MIGUEL, and SHARLEEN OSPINA. "EVALUACIÓN, COMPARACIÓN Y COMPORTAMIENTO DE LOS PRINCIPALES INDICADORES FINANCIEROS DE LAS PYMES DEL SECTOR INMOBILIARIO DE LA ECONOMÍA COLOMBIANA PARA LOS AÑOS 2016 – 2018." Pensamiento Republicano 11 (July 31, 2019): 127–52. http://dx.doi.org/10.21017/pen.repub.2019.n11.a60.
Full textAbstract:
Deficiencies in strategic, administrative, productive or financial performance make many organizations more vulnerable to financial imbalance, generally characterized by insolvency and low liquidity. It is therefore necessary for management to have a constant and thorough knowledge of the economic and financial condition of its sector, which allows it to detect errors in time and apply the necessary corrections, predict the future and make better decisions. The financial analysis or diagnosis is the most effective tool to evaluate the economic and financial performance of a company throughout a specific exercise and thus, to compare its results with those of other companies in the same sec- tor and with similar characteristics. The evaluation of the indicators of the SME real estate sector is not carried out, and as a consequence there is no tool that allows an adequate decision making by the top manage- ment of a company. On the other hand, it is possible to evidence that the exogenous variables that affect the real state sector such as the devaluation of the peso against the dollar influence many indicators of the EEFF. The real estate sector in Colombia has had a contraction in the GDP in the order of -2.1% for the years 2017-2018, all this is due to excess supply, a phenomenon that occurs in both high and low income strata; there is a supply that is exceeding demand in the sector and this affects the sector significantly.
46
Jani, Kunal, Vibhaw Srivastava, Preeti Sharma, Aruna Vir, and Avinash Sharma. "Easy Access to Antibiotics; Spread of Antimicrobial Resistance and Implementation of One Health Approach in India." Journal of Epidemiology and Global Health 11, no. 4 (September 28, 2021): 444–52. http://dx.doi.org/10.1007/s44197-021-00008-2.
Full textAbstract:
AbstractAntimicrobial resistance (AMR) is a global public health concern because of its fast spread. India, one of the world’s top consumer of antibiotics and second most populated country has its unique constraints of social, cultural and economic strata. The continual self-medication, use of antibiotics for the growth promotion in animals, and accumulation of residual antibiotics in the environment challenge the implementation of AMR containment policy. Hence, the present review attempts to delineate the influence of antibiotics abuse on the human, animal and environmental health under the realm of one health. It was based on the literature search using public databases to highlight the rapid surge in the burden of AMR in India affecting various sectors and/or ecosystems in India. It was found that the irrational and overuse of antibiotics in different sectors have led to the emergence of extended antimicrobial resistance wherein the environment acts as a reservoir of antibiotic resistance genes (ARGs); completing the cycle of contamination and recontamination. There are efforts by government policy makers to reduce the burden of AMR in the country to reduce the health risks, through the One Health approach. Parallel efforts in educating healthcare professionals, strict legislation for pharmacies and pharmaceutical companies should be prioritize. At the same time surveillance of newly emerged AMR pathogens, prioritising research focusing on AMR, and awareness camps or programs among the local population is critical while addressing the consequences of spared of AMR in India.
47
Chatalov, Athanas. "Quartz arenites and laterites in the Moesian Group (Upper Triassic), northwestern Bulgaria: possible evidence for the effect of the Carnian Humid Episode." Geologica Balcanica 46, no. 1 (July 2017): 3–25. http://dx.doi.org/10.52321/geolbalc.46.1.3.
Full textAbstract:
Quartz-rich sandstones and ironstone crusts occur in the lowermost part of the Upper Triassic Moesian Group exposed in the western Balkanides. On the basis of performed field studies, micropetrography, X-ray diffraction, and major-element chemistry, these deposits are defined as first-cycle quartz arenites and laterites, respectively. The former were deposited in an alluvial environment, while the latter developed in gravel-dominated fluvial sediments. The main control on their formation was warm to hot humid climate conditions combined with low relief, quiescent tectonic setting, mixed source area, and slow sedimentation rate. The decreasing compositional maturity of the sandstones forming the Glavatsi Member (quartz arenites→feldsarenites→litharenites), the disappearance of the lateritic crusts upwards in the continental succession, and the presence of thick overlying fluvial and playa deposits in the Komshtitsa Formation (or Chelyustnitsa Formation) reflect gradual transition from humid to subhumid climate, and then to persistent semi-arid climate regime. This irreversible trend correlates with other Upper Triassic strata deposited in the Western Tethys realm and adjacent areas. The coeval formation of quartz arenites and laterites must have been related to the most distinctive climate change during the Triassic, i.e., the global Carnian Humid Episode. The new results and interpretations appear to be the first geological record for the effect of pronounced mid-Carnian humidity reported from Eastern Europe. They also present indirect sedimentological evidence for the stratigraphical range of the Moesian Group in NW Bulgaria.
48
Webster, G. D., James W. Haggart, Carrie Saxifrage, Barry Saxifrage, Christian Gronau, and Aileen Douglas. "Globally significant Early Permian crinoids from the Mount Mark Formation in Strathcona Provincial Park, Vancouver Island, British Columbia — preliminary analysis of a disappearing fauna." Canadian Journal of Earth Sciences 46, no. 9 (September 2009): 663–74. http://dx.doi.org/10.1139/e09-039.
Full textAbstract:
Strata of the Mount Mark Formation, Buttle Lake Group, exposed in the vicinity of Marble Peak in Strathcona Provincial Park, central Vancouver Island, contain a diverse Early Permian crinoid fauna. This is the first Permian fauna containing crowns and cups recognized from Wrangellia terrane. The fauna contains representatives of each of the major Paleozoic crinoid subclasses: Camerata, Disparida, and Cladida. Specimens were observed and photographed between 2004 and 2008. No specimens were collected in adherence to regulations of Stratcona Provincial Park. Preliminary identifications recognize several new genera and species within the fauna, but they are not named or described lacking specimens for repository. A minimum of 24 species are judged to be in the fauna, making it the second most diverse Permian fauna known from North America. Identified genera suggest a greater relationship to North American faunas than to Paleotethyan faunas, suggesting Wrangellia was closer to North America than to the Paleotethyan realm during Early Permian time. Exposures of the Mount Mark Formation in the vicinity of Marble Peak are undergoing karstification, and specimens are being lost under the harsh weathering conditions. Observations of individual specimens over a five-year interval found that morphologic details critical for identification are being lost at an alarming rate. It is recommended that sufficient specimens in the fauna should be collected as soon as possible for identification and analysis. These specimens should be preserved for future reference and could form an educational display in the Strathcona Provincial Park headquarters.
49
Lillegraven, Jason A. "Stratigraphic relationships along the monoclinal eastern base of Bald Ridge and northwestern edge of Wyoming’s Bighorn Basin, U.S.A." Rocky Mountain Geology 54, no. 2 (December 1, 2019): 47–95. http://dx.doi.org/10.24872/rmgjournal.54.2.47.
Full textAbstract:
ABSTRACT This geologic study is focused on a less than 5 square-mile (ca. 13 km2) tract of public land in northwestern Wyoming, 8 miles (12.9 km) south-southwest of the small town of Clark in Park County. The study area is south of Clarks Fork of Yellowstone River along the eastern base of the topographic feature called Bald Ridge, also known structurally as Dead Indian monocline. Since the Middle Eocene, the study area has been along the northwestern margin of the Bighorn Basin. Prior to that time, the study area existed near the west–east center of the basin. Bald Ridge became elevated late in the Laramide orogeny (no older than the Early Eocene) through east-directed faulting of basement rocks via the extensive Line Creek–Oregon Basin thrust system. As that active faulting occurred, the overlying Phanerozoic strata (Lower Cambrian through Lower Eocene) responded with numerous west-directed, out-of-the-basin thrusts as a new western-basin margin developed along the eastern realm of the newly born Absaroka volcanic field. Most of that deformation occurred after deposition of uppermost levels of the Lower Eocene Willwood Formation. The key purpose of the present paper was to improve the accuracy of mapping of the Jurassic into Eocene stratigraphy along the newly restricted, northwestern edge of Wyoming’s Bighorn Basin. The stratigraphic column in a north–south band along the eastern flank of the Beartooth Mountains and continuing southward into the present study area was markedly deformed and deeply eroded late during the Laramide orogeny. The present small, more southerly study area is structurally and erosionally simpler than its more northerly equivalent. Thus, its study adds important geological information to the history of the northern Cody Arch, a convex-westward string of related basement-involved uplifts extending southward to southwest of the city of Cody. Progressively steepening eastward dips of strata characterize a west-to-east transect from the summit of Bald Ridge (capped by the shallowly dipping, Mississippian Madison Limestone) to the western edge of strongly overturned outcrops of the Eocene Willwood Formation. The Upper Cretaceous Meeteetse Formation is the stratigraphic horizon at which the dips attain vertical or slightly overturned orientations. All consequential faults within the newly mapped area are thrusts, and they show generally westward (out-of-the-basin) displacements. Despite those west-directed displacements, their primary cause was tectonic shortening at depth below Bald Ridge that was directed to the northeast or east-northeast. During the Laramide orogeny, certain thrust planes within the east-dipping Phanerozoic rock column cut down-section stratigraphically (but uphill relative to Earth’s surface) and thereby placed younger strata upon older. The cumulative result, as recognized at several levels within the present area of study, was marked thinning of the total section. For example, surface exposures of the mostly Paleocene Fort Union Formation, 4,000 feet (1,219 m) thick only 7 miles (11.3 km) to the east, was completely eliminated from the local surface stratigraphy by that means. The northern end of Bald Ridge is formed by the highly asymmetric Canyon Mouth anticline. That structure differs strongly in the attitude of its hinge line from the general east-northeast dip of strata cloaking Bald Ridge. The Canyon Mouth anticline’s hinge line plunges steeply to the southeast, and dips on its northeastern flanks are vertical to partly overturned. Surprisingly, hinge lines and flanks of all other anticlinal/synclinal structures recognized within the present map area share those same orientations with Canyon Mouth anticline. These consistent but unexpected differences in orientation from unfolded strata may represent very late events in the history of Laramide strain vectors across the study area. Working in northern parts of this study area, an independent group determining radiometric ages of detrital-zircon grains reported close agreements in age with their host localities in the Early Cretaceous Mowry Shale and Frontier Formation. However, under the present paper’s interpretation of the local stratigraphy, the other workers misidentified formational hosts for all three samplings. That resulted in age-determination errors of depositional history within the Upper Cretaceous section of as much as 28.8 million years.
50
Suyoga, I. Putu Gede, Made Adi Adi Widyatmika, and Ni Ketut Ayu Juliasih. "Bali Traditional Architecture: Sustainability from the Perspective of Capital Concept." International Journal of Interreligious and Intercultural Studies 3, no. 2 (December 3, 2020): 50–57. http://dx.doi.org/10.32795/ijiis.vol3.iss2.2020.1090.
Full textAbstract:
This study aims to reveal the sustainability of Balinese traditional residential architectural practices which are based on the provisions of traditional ethnic Balinese social stratification and refers to the capital ownership in Generative Structural Theory from Pierre Bourdieu (economic, cultural, social and symbolic). At present, there are dynamics ownership and capital conversion in the traditional social strata which affect the sustainability of traditional residential architecture practices. The traditional Balinese residential architecture in this study is understood to be the spatial layout and traditional residential buildings of the Middle Bali era. Its sustainability today is seen from the concept of capital in the perspective of Bourdieu’s theory. The basic assumption of Bourdieu’s theory is basically that humans are in the field of social struggle to emerge victorious by competing with one another. This study is a qualitative research with interpretative descriptive method. Primary data were obtained from selected informants (purposive) and from field observations, as well as secondary data from the literature. The study findings show that traditional residential architecture practices in the Middle Bali era were strongly influenced by capital ownership (economic, cultural, social, and symbolic) with various forms of conversion to traditional Balinese aristocratic (triwangsa). Development at this time has opened the opportunity to control various capital for ordinary community (jabawangsa), so that the realm of Balinese traditional housing becomes a medium of struggle as well as a symbol of success in social struggle. On the other hand, the contestation of Balinese traditional residential architectural practices is a sustainability in the arena of social struggle within Balinese society today.