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Добірка наукової літератури з теми "Upper Khabur"

Автор: Grafiati

Опубліковано: 10 березня 2023

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Статті в журналах з теми "Upper Khabur"

1

NISHIAKI, Yoshihiro. "The Late Halafian Lithic Industry of Tell Kashkashok I, the Upper Khabur, Syria." Orient 53 (September 30, 2018): 1–21. http://dx.doi.org/10.5356/orient.53.1.

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2

Deckers, Katleen, and Simone Riehl. "Fluvial environmental contexts for archaeological sites in the Upper Khabur basin (northeastern Syria)." Quaternary Research 67, no. 3 (May 2007): 337–48. http://dx.doi.org/10.1016/j.yqres.2006.11.005.

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AbstractToday the eastern tributaries of the Upper Khabur run dry during the summer and the landscape is devoid of trees. This picture is misleading when we try to understand archaeological sites within their former environmental context. Interdisciplinary geomorphological, archaeobotanical and ostracod research on a sequence from the Wadi Jaghjagh indicates that relatively stable, perennial flow velocities occurred during the mid 4th to mid-3rd millennium BC. Evidence was found for a gallery forest and swamp belt along the Jaghjagh during the mid-4th millennium BC. Oak park woodland was present within the region in the 3rd millennium BC and probably up to at least the 3rd century AD. Shortly after 2500 BC, Jaghjagh stream velocities probably decreased or the stream bed had changed its location. Later deposits, possibly dating to the 5th century BC, indicate similar, rather stable flow of the Jaghjagh. More recently however, about ca. AD 900 or afterwards, a flashflood-like regime occurred, which may relate to deforestation. The Wadi Khanzir sediment archives reflect the flashy intermittent regime of this stream, like it still is today, with flashflood evidence dating to the first half of the Holocene and probably dating to approximately AD 400 or later. Along the Jarrah, topsoil was eroded and redeposited by the wadi sometime between 1300 and 600 BC. This may have been caused by the intensive resettlement program of this region around 800 BC. Between about 600 and 300 BC 1.5 m of clay was deposited on the plain.

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3

Deckers, Katleen, and Simone Riehl. "Resource Exploitation of the Upper Khabur Basin (NE Syria) during the 3rd Millennium BC." Paléorient 34, no. 2 (2008): 173–89. http://dx.doi.org/10.3406/paleo.2008.5261.

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4

D’Agostino, Anacleto. "The Assyrian–Aramaean interaction in the Upper Khabur: the archaeological evidence from Tell Barri iron age layers." Syria, no. 86 (November 1, 2009): 17–41. http://dx.doi.org/10.4000/syria.507.

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5

Nishiaki, Yoshihiro A., and Marie Le Mière. "The oldest pottery Neolithic of Upper Mesopotamia : New evidence from Tell Seker al-Aheimar, the Khabur, northeast Syria." Paléorient 31, no. 2 (2005): 55–68. http://dx.doi.org/10.3406/paleo.2005.5125.

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6

Portillo, Marta, Seiji Kadowaki, Yoshihiro Nishiaki, and Rosa M. Albert. "Early Neolithic household behavior at Tell Seker al-Aheimar (Upper Khabur, Syria): a comparison to ethnoarchaeological study of phytoliths and dung spherulites." Journal of Archaeological Science 42 (February 2014): 107–18. http://dx.doi.org/10.1016/j.jas.2013.10.038.

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7

Restelli, Francesca Balossi. "The local Late Chalcolithic (LC3) occupation at Zeytinli Bahçe (Birecik, Şanli-Urfa): the ceramic production." Anatolian Studies 56 (December 2006): 17–46. http://dx.doi.org/10.1017/s0066154600000739.

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AbstractExcavations and ceramic finds of the Late Chalcolithic 3 (3,700–3,500 BC) from the site of Zeytinli Bahçe, on the Turkish Euphrates, are published and discussed, with particular attention to modes of manufacture in the phase which immediately precedes the introduction of the fast wheel and mass production (middle and late Uruk). In this period, alternative modes of manufacture (coil, mould, wheel) are probable indices of experimentations in response to ever increasing economic and social needs. Ceramic classes and types are also analysed with the aim of understanding inter-regional relations in the period preceding the arrival of Uruk influence. Together with Hacınebi, Zeytinli Bahçe provides important data on Late Chalcolithic developments in the Turkish Euphrates region south of the Taurus. These help distinguish single cultural horizons, but also identify large networks of communication right down to the Iraqi Tigris. Relations of the middle Euphrates area appear to be biased eastwards, towards the Khabur river, whilst direct contacts with the regions north of the Taurus seem absent. However, indirect chronological correlations are made possible by an overview of the general distribution of ceramic typologies in the whole upper Mesopotamia and Taurus regions during the Late Chalcolithic period.

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8

Al-jubori, Falah H. Khalaf, Akram K. Youkhana, Srood F. Naqshabandi, and Dyana A. Bayz. "BIOSTRATIGRAPHIC CORRELATION OF PALEOZOIC ROCKS IN NORTHERN AND WESTREN IRAQ." International Journal of Research -GRANTHAALAYAH 8, no. 3 (May 26, 2020): 315–23. http://dx.doi.org/10.29121/granthaalayah.v8.i3.2020.163.

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The Paleozoic rocks outcropped in northern Iraq (Ora, Chia Zairi section) are biostratigraphically investigated for their microfossils content. Benthonic foraminifera and algal genera characterize the upper part of the section while palynomorphs (Miospores & Acritarchs) dominated the lower part the section which is consist of clastic sediments. The study also include the stratigraphic succession of the section and its correlation to the subsurface sections penetrated in oil and water wells drilled in the western desert of Iraq in order to determine the regional distribution of the economically important formations, either as reservoir or as source rocks for hydrocarbons. Index palynomorphs including many types of Acritarch genera are identified in the Khabour Formation indicate lower Ordovician time (Tremadocian? Arenigian –Llanvirnian: age) The Perispik Formation has been found barren of any type of microfossils and is composed of red clastic rocks. Pollen and Spores are recorded from the "Ore Group" (Kaista, Ora and Harur Formations ) indicate that these rocks are of Upper Devonian – Lower Carboniferous (Famennian – Tournaisian age ) .A Large number of foraminifera and Algal genera are identified in the Chiazairi rocks,these genera and species are indicated the Upper Permian rocks of Thuringian age. The stratigraphic succession of the Paleozoic section studied in northern Iraq indicate that there is a stratigraphic break represents by missing of the Ga'ara Formation (late Carboniferous –early Permian) and Akkas Formation (Silurian) and the upper part of the Khabour Formation (Upper Ordovician).

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9

AL- Hadidy, Dr Aboosh H. "Deliverability of Gas condensate "sandstone reservoir"Khabour Fm. Akkas Field,western Iraq." Journal of Petroleum Research and Studies 2, no. 3 (May 5, 2021): 243–78. http://dx.doi.org/10.52716/jprs.v2i3.58.

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The Khabour Fm. (ordovicain) presents a prospective target for exploration and developiment, as it certains "Gas Condensate" light gravity, low sulfur oil, and sweet gas as proven by Akkas field, in the western desert of Iraq . Gas- condensate project is in depth,hot,low permeability reservoir in the upper K1,K3,K5 sandstone members ,it's well known that the deliverability of gas-condensate wells can be improved by the formation of acondensate bank once a bottomhole pressure drope below the dewpoint. Improving deliverability can be improved by use the techniques as,Fracturing andchemical treatment. The Khabour formation total thickness is 1913m,represntaed by elastic series mainly shaly intercalated with sandstone beds in the lower part and by well developed sandstone beds in the upper part, In Akk-1 which is subdivided into eight members according to sand /shale ratio, the need for accurate estimate for reservoir properties of these member extends to the whole life cycle of a reservoir; detailed simulation and planning of future production which including for discovery , appraisal , planning , development and production from Akkas field.

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10

Abdul-majeed, Yousif Najeeb, Ahmad Abdullah Ramadhan, and Ahmed Jubiar Mahmood. "Petrophysical Properties and Well Log Interpretations of Tertiary Reservoir in Khabaz Oil Field / Northern Iraq." Journal of Engineering 26, no. 6 (June 1, 2020): 18–34. http://dx.doi.org/10.31026/j.eng.2020.06.02.

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The aim of this study is interpretation well logs to determine Petrophysical properties of tertiary reservoir in Khabaz oil field using IP software (V.3.5). The study consisted of seven wells which distributed in Khabaz oilfield. Tertiary reservoir composed from mainly several reservoir units. These units are : Jeribe, Unit (A), Unit (A'), Unit (B), Unit (BE), Unit (E),the Unit (B) considers best reservoir unit because it has good Petrophysical properties (low water saturation and high porous media ) with high existence of hydrocarbon in this unit. Several well logging tools such as Neutron, Density, and Sonic log were used to identify total porosity, secondary porosity, and effective porosity in tertiary reservoir. For Lithological identification for tertiary reservoir units using (NPHI-RHOB) cross plot composed of dolomitic-limestone and mineralogical identification using (M/N) cross plot consist of calcite and dolomite. Shale content was estimated less than (8%) for all wells in Khabaz field. CPI results were applied for all wells in Khabaz field which be clarified movable oil concentration in specific units are: Unit (B), Unit (A') , small interval of Jeribe formation , and upper part of Unit (EB).

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Більше джерел

Дисертації з теми "Upper Khabur"

1

Kumar, Navneet [Verfasser]. "Impacts of Climate change and Land use change on the Water resources of the Upper Kharun Catchment, Chhattisgarh, India / Navneet Kumar." Bonn : Universitäts- und Landesbibliothek Bonn, 2014. http://d-nb.info/1077268912/34.

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2

Shidrang, Sonia. "The early Upper Paleolithic of Zagros : techno-typological assessment of three Baradostian lithic assemblages from Khar Cave (Ghar-e Khar), Yafteh Cave and Pa-Sangar Rockshelter in the Central Zagros, Iran." Thesis, Bordeaux, 2015. http://www.theses.fr/2015BORD0073.

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Comme pour l’Europe, la question de la transition du Paléolithique moyen (MP)au Paléolithique supérieur (UP) concernant l'Asie occidentale est toujours un débat d’actualité, notamment intense dans les domaines de l’archéologie paléolithique et de la paléoanthropologie. Ce changement, ou « transition », a constitué un tournant important pour deux volets de l'évolution humaine : biologique d’une part, culturel d’autre part. La disparition de l'homme de Néandertal et l'expansion généralisée de l'Homme anatomiquement moderne (HAM) ainsi que l'émergence de technologies coïncidant au début du Paléolithique supérieur en Europe et en Asie sud occidentale sont quelques-uns des aspects énigmatiques de cette période dite de transition relative à une tranche de temps comprise entre 45 000 et 30 000 ans. Sans doute, le Moyen-Orient ou l'Asie occidentale constituent-ils une zone clé qui a, de tout temps, concentré une recherche portant sur l'origine de la dispersion de la première large manifestation culturelle des hommes anatomiquement modernes.Ce mémoire s’attache à présenter une synthèse des industries lithiques du Paléolithiquesupérieur ancien du Zagros central (Iran), laquelle constitue une partie importante de laculture matérielle liée à la transition du Paléolithique moyen au Paléolithique supérieur,l'une des étapes cruciales de l'évolution humaine du Proche et Moyen-Orient.Ce projet de thèse a été conçu suivant un ordre chronologique visant à étudier trois assemblages disponibles, correspondant par ailleurs à trois phases du début du Paléolithique supérieur au Zagros appelé également « Baradostien ». L'étude vise à documenter les changements techno-typologiques pour les séquences concernées en même temps qu'elle définit les caractéristiques détaillées de chaque industrie. La méthode visant à reconstituer les chaînes opératoires a été le plus systématiquement possible sollicitée. Elle permet de présenter une image détaillée et réactualisée du Baradostien, ses stratégies de débitage lithique et leur place, leurs importances au travers de la diachronie régionale. Les assemblages lithiques de Ghar-e-Khar sont examinés uniquement dans le but de discuter ses caractéristiques technologiques et la tendance apparemment mélangée de ce début du Paléolithique supérieur / fin du Paléolithique moyen pour la couche intermédiaire MP-UPde ce site. L’industrie lithique de la grotte de Yafteh représentait jusqu’à présent une référence centrale et représentative du Baradostien pour le Zagros central. Les études détaillées de nouveaux assemblages issus de fouilles récentes montre une image plus complexe. Enfin, l'étude de l'assemblage lithique de Pa-Sangar permet de tester la validité de la réinterprétation du Baradostien telle que récemment déduite des travaux menés récemment à Yafteh, mais ici testée pour une série issue d’un site différent
The Middle to Upper Paleolithic transition is an intensely debated topic in Paleolithicarchaeology and paleoanthropology of Western Asia. The disappearing of Neanderthals and the widespread expansion of anatomically modern humans as well as the emergence of Early Upper Paleolithic technologies in Europe and Southwest Asia are just some of the enigmatic aspects of this transitional period which occurred during Marine Isotope Stage 3.The level of our knowledge on the subject of Middle to Upper Paleolithic transitional events is not the same in all regions of Southwest Asia. This thesis presents a synthesis of the EarlyUpper Paleolithic lithic industries of Central Zagros or Baradostian as an important part of the material culture related to this crucial stages of human evolution in western part of Iran. It reviews most important parts of the EUP related data from this region and examines the lithic-based dominant hypothesis of continuity in the Zagros through a moretechnology oriented view and put together all the evidence to present a broader overview of the Early Upper Paleolithic in Zagros and its lithic industrial evolution. Incorporating new information from typo-technological and taphonomical studies of three Baradostian assemblages from Khar cave (Ghar-e Khar), Yafteh cave and Pa-Sangar rockshelter into the existing knowledge, this thesis provides us with a better reconstruction of the Baradostain sequence in the Zagros

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3

ORSI, VALENTINA. "Persistenze e discontinuita' nella tradizione ceramica dell'Alta Mesopotamia tra la fine del Terzo e l'inizio del Secondo millennio a.C.. il contributo degli scavi di Tell Barri e Tell Mozan (Siria)." Doctoral thesis, 2010. http://hdl.handle.net/2158/560486.

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Il periodo tra la fine del III e l'inizio del II millennio a.C. in Alta Mesopotamia rappresenta nella storia e nell'archeologia del Vicino Oriente Antico una 'Media Aetas', un'età oscura tra la fioritura delle culture urbane del Bronzo Antico a metà del III millennio a.C. e lo sviluppo degli stati amorrei del Bronzo Medio, alla fine del XIX sec. a.C. L'identificazione nella sequenza archeologica di Tell Barri, l'antica città di Kahat, dell'orizzonte ceramico coevo alla 'crisi urbana' che precede la diffusione della ceramica dipinta del Khabur, associata ad un nuovo fenomeno di sedentarizzazione, permette di ridefinire la cronologia degli eventi nella regione, e di delineare i processi di interazione tra le diverse realtà sociali alto mesopotamiche in quella fase formativa che sta alla base del successivo sviluppo culturale di II millennio a.C.

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Частини книг з теми "Upper Khabur"

1

Crevecoeur, I. "The Upper Paleolithic Human Remains of Nazlet Khater 2 (Egypt) and Past Modern Human Diversity." In Modern Origins, 205–19. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-2929-2_14.

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2

Kadowaki, Seiji. "Ahmarian or Levantine Aurignacian? Wadi Kharar 16R and New Insights into the Upper Palaeolithic Lithic Technology in the Northeastern Levant." In The Middle and Upper Paleolithic Archeology of the Levant and Beyond, 105–16. Singapore: Springer Singapore, 2017. http://dx.doi.org/10.1007/978-981-10-6826-3_8.

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3

"The Upper Khabur and the Upper Tigris Valleys during the Late Bronze Age: Settlements and Ceramic Horizons." In The Archaeology of Political Spaces, 169–200. De Gruyter, 2014. http://dx.doi.org/10.1515/9783110266405.169.

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4

Palmisano, Alessio. "Geopolitical Patterns and Connectivity in the Upper Khabur Valley in the Middle Bronze Age." In Tradition and Innovation in the Ancient Near East, 369–80. Penn State University Press, 2015. http://dx.doi.org/10.5325/j.ctv1bxgx2w.35.

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5

Palmisano, Alessio. "Geopolitical Patterns and Connectivity in the Upper Khabur Valley in the Middle Bronze Age." In Tradition and Innovation in the Ancient Near East, 369–80. Penn State University Press, 2015. http://dx.doi.org/10.1515/9781575063584-033.

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6

"The Settlement Pattern of the Western Upper Khabur from the Old Babylonian Period to the End of the Mittani Era." In Constituent, Confederate, and Conquered Space, 213–46. De Gruyter, 2014. http://dx.doi.org/10.1515/9783110266412.213.

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7

von Dassow, Eva. "Mittani and Its Empire." In The Oxford History of the Ancient Near East: Volume III, 455–528. Oxford University Press, 2022. http://dx.doi.org/10.1093/oso/9780190687601.003.0029.

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Анотація:

The kingdom of Mittani, also known as Hanigalbat, the Hurrian kingdom, and Naharina, was established in the area of the upper Khabur River in the late sixteenth century BC. Having first taken form as Hanigalbat, this kingdom incorporated immigrants from beyond the Zagros into local populations among whom speakers of Hurrian predominated. Mittani acquired an empire extending across northern Mesopotamia, Syria, and eastern Anatolia during the fifteenth century BC, vying with New Kingdom Egypt as one of two “superpowers” in the Near East. It later lost this status, and its empire, in competition with Assyria and Hatti, then struggled along under the name Hanigalbat until it was extinguished in the thirteenth century BC. This chapter surveys the sources and covers the history of Mittani from its obscure origins through the growth of its empire to its dismemberment and demise. The chapter also examines the role attributed to speakers of an Indo-Aryan language, horse-drawn chariotry as a factor in the emergence of a new political and social order, and the governance of Mittani’s empire. During its floruit, the kingdom of Mittani appears to have experimented with diverse models of imperial rule, pioneered the differentiation of citizenship between sovereign and subject states, and promoted the differentiation of social classes according to status and socioeconomic capacity. Meanwhile, its culture featured an efflorescence of new styles and technologies in diverse media, notably including glass manufacture. Some of the innovations survived Mittani’s demise, as did some Hurrian literature, transmitted and transformed by Assyrian, Hittite, and other hands.

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8

"UPPER-WADI SETTLEMENTS." In The Tangible and Intangible Cultural Landscape of Wadi Bani Kharus, 376–415. Archaeopress Publishing Ltd, 2020. http://dx.doi.org/10.2307/j.ctv1ddckx6.18.

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9

"UPPER-WADI SETTLEMENTS." In The Tangible and Intangible Cultural Landscape of Wadi Bani Kharus, 376–415. Archaeopress Publishing Ltd, 2020. http://dx.doi.org/10.2307/j.ctv1ddckx6.18.

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10

Trinkaus, Erik, Alexandra P. Buzhilova, Maria B. Mednikova, and Maria V. Dobrovolskaya. "The Sunghir Human Hands." In The People of Sunghir. Oxford University Press, 2014. http://dx.doi.org/10.1093/oso/9780199381050.003.0016.

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As the interface between the body and technology, in all of its myriad forms, the skeletal hand morphology of Late Pleistocene humans has received increasing attention since the work of Sarasin (1932) and especially Musgrave (1970, 1971, 1973), as paleoanthropologists have documented a series of contrasts between archaic Homo and recent human hand bones (e.g., Vlček 1975; Trinkaus 1983b; Vandermeersch 1991; Niewoehner et al. 1997; Niewoehner 2001, 2008; Crevecoeur 2008; Lorenzo 2007; Trinkaus in press). However, since there were major changes in human technology between the Middle and Upper Paleolithic, and especially with the Mid Upper Paleolithic (MUP), the comparisons of concern should be between late archaic humans and early modern humans. For the Early Upper Paleolithic, the latter include relatively complete hand remains from Nazlet Khater 2 and scattered hand bones from Tianyuan 1 and Brassempouy (Henry-Gambier et al. 2004; Crevecoeur 2008; Shang and Trinkaus 2010). There are then relatively abundant hand remains from the MUP (Verneau 1906; Matiegka 1938; Mallegni et al. 1999; Sládek et al. 2000; Trinkaus 2006c; Trinkaus et al. 2010, 2014), including some immature ones (Mallegni and Parenti 1973; Sergi et al. 1974; Trinkaus et al. 2002b). Yet few of them have been described in detail. In this context, the Sunghir manual remains are described and select aspects are compared across Late Pleistocene samples (principally features that appear to change with the emergence of modern humans). For these descriptions and comparisons, the Sunghir 1 hand bones are paleontologically well preserved. Of the 54 bones potentially present for Sunghir 1 (not counting pollical sesamoid bones), 49 are known, and none sustained more than minor marginal erosion. The originally missing bones include one pisiform bone and four distal phalanges from the ulnar digits. During and after excavation, the right and left hands were mixed, so that the bones have been sorted based on morphology and (for the ulnar middle and distal phalanges) size.

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Тези доповідей конференцій з теми "Upper Khabur"

1

Sivalneva, O. V., A. V. Postnikov, V. V. Poshibaev, E. K. Idrisova, O. A. Antipova та A. S. Kuznecov. "Сomparative Lithological Characterization of Rocks from Upper Part of the Khadum Formation in the East Caucasian Region". У EAGE/SPE Workshop on Shale Science 2019. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201900470.

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2

Федосеев, Н. Ф., and Л. Ю. Пономарев. "Settlement of early Byzantine time at the Kyz-Aul necropolis." In Древности Боспора. Crossref, 2018. http://dx.doi.org/10.25681/iaras.2018.978-5-94375-251-3.257-281.

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Necropolis Kyz-Aul is located on the Black Sea coast, 1 km to the south-east of the village. Yakovenkovo. In 1930, 1979–1983, 1985, 1995, 1997, 2000, 2005–2006, 2015–2017, he was investigated by Yu. Martti, O. Chevelev, N. Sudarev and N. Fedoseev. Separate burials date back to the II–I BC, the burial of the I–III AD the most recent burials, apparently, were committed in the IV–V AD. In the VI – third quarter of the VII century AD on the territory of the already abandoned necropolis, a small settlement was located. Its cultural stratum is traced on all sites that have been followed in the last decade. As living quarters, the looted crypts of the 1st–3rd centuries AD were adapted, consisting of one or two funerary cells and built of massive blocks of limestone (№ 6, 7, 9, 10). With exception of the crypts of the poorly preserved pit of the semidugout (?) other residential and household buildings on the necropolis could not be fixed. One child burial also belongs to the same period. The most well-preserved living room in the crypt number 6. In one of its funerary cells housed five household pits and heating devices, including a fireplace, reminiscent of the design of the fireplace. In the other crypts, the interior details of the “underground” dwellings have not been preserved. In the “Khazar” time burial chamber crypts were adapted for the maintenance of small cattle. The time of the early Byzantine settlement on the necropolis dates numerous finds of amphorae. The upper date was determined thanks to the coin of 674 Constantine IV Pogonat. In addition, a ring with the image of an archangel was found, an analogy of which is known in the burial complexes of the 7th century. Unfortunately, the area and location of the necropolis of this settlement is not yet established. Cannot be reconstructed and its layout. It is difficult to reconstruct the interior of the “underground” dwellings themselves, since the crypts were reused in the “Khazar” period. In addition, no other settlements of this time were found on the ancient necropolises of the Kerch Peninsula

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