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Bibliografias temáticas / Molasse basin

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Literatura científica selecionada sobre o tema "Molasse basin"

Autor: Grafiati

Publicado: 21 de setembro de 2024

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Artigos de revistas sobre o assunto "Molasse basin"

1

Pashko, Pandeli. "Morave Mt Oligocene-Middle Miocene succession of Albanian-Thessalian Basin". Bulletin of the Geological Society of Greece 52, n.º 1 (28 de setembro de 2018): 1. http://dx.doi.org/10.12681/bgsg.15837.

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The Morava Mountain Oligocene-Middle Miocene molasse deposits take part in the Albanian-Thessalian Basin, which developed NW-SE from eastern Albania to Thessaly in Greece, where it is called as Mesohellenic Basin. The 4.5 km thick basin infill is subdivided into three molasse cycles separated by two regional unconformities at the Eocene/Oligocene and Aquitanian/Burdigalian boundaries. The Morava Mountain Oligocene-Middle Miocene molase, ~ 3500 m thick, represents an exposed continuous, rich in fossil fauna succession. Six stratigraphic sections were studied and measured.

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2

Akgiin, Funda, e Hasan Sözbilir. "A palynostratigraphic approach to the SW Anatolian molasse basin: Kale-Tavas molasse and Denizli molasse". Geodinamica Acta 14, n.º 1-3 (janeiro de 2001): 71–93. http://dx.doi.org/10.1080/09853111.2001.11432436.

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3

Akgün, F. "A palynostratigraphic approach to the SW Anatolian molasse basin: Kale–Tavas molasse and Denizli molasse". Geodinamica Acta 14, n.º 1-3 (maio de 2001): 71–93. http://dx.doi.org/10.1016/s0985-3111(00)01054-8.

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4

Mamengko, David Victor, Yoga B.Sendjadja, Budi Mulyana, Hermes Panggabean, Iyan Haryanto, Eko Budi Lelono, Juwita Trivianty Musu e Panuju Panuju. "Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara". Jurnal Geologi dan Sumberdaya Mineral 20, n.º 1 (25 de fevereiro de 2019): 37. http://dx.doi.org/10.33332/jgsm.2019.v20.1.37-47.

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North Papua Basin is a fore arc basin located in northern coastal of Papua Island. This basin filled by Middle-Upper Miocene turbidite sediment and overlied by Upper Miocene – Quarternary clastic sediment. Upper Miocene – Quaternary clastic sediments (Mamberamo Formation) composed by interbedding conglomerate, sandstone and shale as molasses deposit. A detailed stratigraphic study was performed to identify facies and its association of the Mamberamo Formation to that give a new perspective on the characteristics and development of facies succession of Lower Mamberamo Formation. Result shows that the Lower Mamberamo Formation consists of three facies: A) cross bedding sandstone (subtidal), B) heterolothic silty shale (intra-tidal), C) carbonaceous shale (supra-tidal) deposited on Late Miocen to Plio-Pleistocene during centra range orogeny (syn-orogeny) as molasses deposits.Keywords: Fore arc basin, North Papua Basin, Mamberamo Formation, molasse deposits.

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Mamengko, David Victor, Yoga B.Sendjadja, Budi Mulyana, Hermes Panggabean, Iyan Haryanto, Eko Budi Lelono, Juwita Trivianty Musu e Panuju Panuju. "Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara". Jurnal Geologi dan Sumberdaya Mineral 20, n.º 1 (25 de fevereiro de 2019): 37. http://dx.doi.org/10.33332/jgsm.geologi.20.1.37-47.

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North Papua Basin is a fore arc basin located in northern coastal of Papua Island. This basin filled by Middle-Upper Miocene turbidite sediment and overlied by Upper Miocene – Quarternary clastic sediment. Upper Miocene – Quaternary clastic sediments (Mamberamo Formation) composed by interbedding conglomerate, sandstone and shale as molasses deposit. A detailed stratigraphic study was performed to identify facies and its association of the Mamberamo Formation to that give a new perspective on the characteristics and development of facies succession of Lower Mamberamo Formation. Result shows that the Lower Mamberamo Formation consists of three facies: A) cross bedding sandstone (subtidal), B) heterolothic silty shale (intra-tidal), C) carbonaceous shale (supra-tidal) deposited on Late Miocen to Plio-Pleistocene during centra range orogeny (syn-orogeny) as molasses deposits.Keywords: Fore arc basin, North Papua Basin, Mamberamo Formation, molasse deposits.

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6

Mamengko, David Victor, Yoga B.Sendjadja, Budi Mulyana, Hermes Panggabean, Iyan Haryanto, Eko Budi Lelono, Juwita Trivianty Musu e Panuju Panuju. "Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara". Jurnal Geologi dan Sumberdaya Mineral 20, n.º 1 (25 de fevereiro de 2019): 37. http://dx.doi.org/10.33332/jgsm.geologi.v20i1.399.

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North Papua Basin is a fore arc basin located in northern coastal of Papua Island. This basin filled by Middle-Upper Miocene turbidite sediment and overlied by Upper Miocene – Quarternary clastic sediment. Upper Miocene – Quaternary clastic sediments (Mamberamo Formation) composed by interbedding conglomerate, sandstone and shale as molasses deposit. A detailed stratigraphic study was performed to identify facies and its association of the Mamberamo Formation to that give a new perspective on the characteristics and development of facies succession of Lower Mamberamo Formation. Result shows that the Lower Mamberamo Formation consists of three facies: A) cross bedding sandstone (subtidal), B) heterolothic silty shale (intra-tidal), C) carbonaceous shale (supra-tidal) deposited on Late Miocen to Plio-Pleistocene during centra range orogeny (syn-orogeny) as molasses deposits.Keywords: Fore arc basin, North Papua Basin, Mamberamo Formation, molasse deposits.

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7

Mamengko, David Victor, Yoga B.Sendjadja, Budi Mulyana, Hermes Panggabean, Iyan Haryanto, Eko Budi Lelono, Juwita Trivianty Musu e Panuju Panuju. "Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara". Jurnal Geologi dan Sumberdaya Mineral 20, n.º 1 (25 de fevereiro de 2019): 37. http://dx.doi.org/10.33332/jgsm.v20i1.399.

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North Papua Basin is a fore arc basin located in northern coastal of Papua Island. This basin filled by Middle-Upper Miocene turbidite sediment and overlied by Upper Miocene – Quarternary clastic sediment. Upper Miocene – Quaternary clastic sediments (Mamberamo Formation) composed by interbedding conglomerate, sandstone and shale as molasses deposit. A detailed stratigraphic study was performed to identify facies and its association of the Mamberamo Formation to that give a new perspective on the characteristics and development of facies succession of Lower Mamberamo Formation. Result shows that the Lower Mamberamo Formation consists of three facies: A) cross bedding sandstone (subtidal), B) heterolothic silty shale (intra-tidal), C) carbonaceous shale (supra-tidal) deposited on Late Miocen to Plio-Pleistocene during centra range orogeny (syn-orogeny) as molasses deposits.Keywords: Fore arc basin, North Papua Basin, Mamberamo Formation, molasse deposits.

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8

Bachmann, G. H., M. Müller e K. Weggen. "Evolution of the Molasse Basin (Germany, Switzerland)". Tectonophysics 137, n.º 1-4 (junho de 1987): 77–92. http://dx.doi.org/10.1016/0040-1951(87)90315-5.

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9

Garefalakis, Philippos, e Fritz Schlunegger. "Tectonic processes, variations in sediment flux, and eustatic sea level recorded by the 20 Myr old Burdigalian transgression in the Swiss Molasse basin". Solid Earth 10, n.º 6 (19 de novembro de 2019): 2045–72. http://dx.doi.org/10.5194/se-10-2045-2019.

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Abstract. The stratigraphic architecture of the Swiss Molasse basin, situated on the northern side of the evolving Alps, reveals crucial information about the basin's geometry, its evolution, and the processes leading to the deposition of the siliciclastic sediments. Nevertheless, the formation of the Upper Marine Molasse (OMM) and the controls on the related Burdigalian transgression have still been a matter of scientific debate. During the time period from ca. 20 to 17 Ma, the Swiss Molasse basin was partly flooded by a shallow marine sea striking SW–NE. Previous studies have proposed that the transgression occurred in response to a rise in global sea level, a reduction of sediment flux, or an increase in tectonically controlled accommodation space. Here, we readdress this problem and extract stratigraphic signals from the Burdigalian molasse deposits that can be related to changes in sediment supply rate, variations in the eustatic sea level, and subduction tectonics. To achieve this goal, we conducted sedimentological and stratigraphic analyses of several sites across the entire Swiss Molasse basin. Field investigations show that the transgression and the subsequent evolution of the Burdigalian seaway was characterized by (i) a deepening and widening of the basin, (ii) phases of erosion and non-deposition during Lower Freshwater Molasse (USM), OMM, and Upper Freshwater Molasse (OSM) times, and (iii) changes in along-strike drainage reversals. We use these changes in the stratigraphic record to disentangle tectonic and surface controls on the facies evolution at various scales. As the most important mechanism, rollback subduction of the European mantle lithosphere most likely caused a further downwarping of the foreland plate, which we use to explain the deepening and widening of the Molasse basin, particularly at distal sites. In addition, subduction tectonics also caused the uplift of the Aar massif. This process was likely to have shifted the patterns of surface loads, thereby resulting in a buckling of the foreland plate and influencing the water depths in the basin. We use this mechanism to explain the establishment of distinct depositional settings, particularly the formation of subtidal shoals wherein a bulge in relation to this buckling is expected. The rise of the Aar massif also resulted in a reorganization of the drainage network in the Alpine hinterland, with the consequence that the sediment flux to the basin decreased. We consider this reduction in sediment supply to have amplified the tectonically controlled deepening of the Molasse basin. Because the marine conditions were generally very shallow, subtle changes in eustatic sea level contributed to the formation of several hiatuses that chronicle periods of erosion and non-sedimentation. These processes also amplified the tectonically induced increase in accommodation space during times of global sea level highstands. Whereas these mechanisms are capable of explaining the establishment of the Burdigalian seaway and the formation of distinct sedimentological niches in the Swiss Molasse basin, the drainage reversal during OMM times possibly requires a change in tectonic processes at the slab scale, most likely including the entire Alpine range between the Eastern and Central Alps. In conclusion, we consider rollback tectonics to be the main driving force controlling the transgression of the OMM in Switzerland, with contributions by the uplift of individual crustal blocks (here the Aar massif) and by a reduction of sediment supply. This reduction of sediment flux was likely to have been controlled by tectonic processes as well when basement blocks became uplifted, thereby modifying the catchment geometries. Eustatic changes in sea level explain the various hiatuses and amplified the deepening of the basin during eustatic highstand conditions.

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Reinecker, John, Mark Tingay, Birgit Müller e Oliver Heidbach. "Present-day stress orientation in the Molasse Basin". Tectonophysics 482, n.º 1-4 (fevereiro de 2010): 129–38. http://dx.doi.org/10.1016/j.tecto.2009.07.021.

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Mais fontes

Teses / dissertações sobre o assunto "Molasse basin"

1

Bass, Jonathan. "The sedimentology and basin evolution of the Upper Marine Molasse of the Rhone-Alp region France". Thesis, University of Oxford, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.302955.

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2

Seithel, Robin Jonas [Verfasser], e T. [Akademischer Betreuer] Kohl. "Geomechanical characterization of geothermal reservoirs in the Bavarian Molasse Basin / Robin Jonas Seithel ; Betreuer: T. Kohl". Karlsruhe : KIT-Bibliothek, 2021. http://d-nb.info/1238148468/34.

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3

Stäuble, Martin Peter. "Seismic reflection profiling from the molasse basin into the Alps of Eastern Switzerland : processing, interpretation and modeling /". [S.l : s.n.], 1990. http://www.ub.unibe.ch/content/bibliotheken_sammlungen/sondersammlungen/dissen_bestellformular/index_ger.html.

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Diss. Phil.-naturwiss. Fak. Bern, 1990.
Enth. Sonderabdrucke: Tectonics vol.9/6: 1327-1355 (1990), Annales tectonicae vol. V/1 3-17 (1991), Eclogae geologicae Helvetiae vol.84/1 151-175 (1991), und Tectonics vol.12 (1993).

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4

Huet, Bastien. "Dynamique des bassins d'avant-pays et collision dans les Alpes de l'Ouest : sources, routage et bilans sédimentaires". Electronic Thesis or Diss., Sorbonne université, 2024. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2024SORUS153.pdf.

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La formation du bassin d'avant pays ouest alpin résulte de la collision alpine à partir de ~34 Ma et de l'exhumation des Alpes internes au cours de l'Oligocène et des Alpes externes au Miocène. Son développement est divisé en deux phases distinctes : un bassin sous-alimenté entre l'Eocène et le Rupélien moyen et un bassin sur-alimenté à partir du Rupélien supérieur et jusqu'à la fin du Miocène. L'évolution de la sédimentation et le calendrier source to sink au cours de cette deuxième phase sont encore peu documentés. Le but de ce travail de thèse est d'apporter de nouvelles données et de mieux comprendre le développement de ce bassin. Ce manuscrit est constitué de trois volets principaux. Le premier se focalise sur la réorganisation du routage sédimentaire entre l'Eocène et le Miocène inférieur. Pour la première fois, un calendrier chronostratigraphique détaillé de tous les bassins oligocènes du SE de la France est proposé via l'acquisition de nouvelles données de terrain et de biostratigraphie, ainsi que la réinterprétation de données de subsurface. Ce travail a permis de mettre en évidence le rôle déterminant de l'orogenèse pyrénéo-provençale qui favorise l'export de matériel alpin en dehors du foredeep dès le Rupélien supérieur et de l'ECRIS qui créé des zones subsidentes dans la vallée du Rhône dès le Priabonien influençant le reste de la sédimentation oligo-miocène. Le prisme orogénique et l'exhumation des Alpes externes a causé, notamment au cours du Chattien, une diminution des apports des Alpes internes dans les bassins oligocènes. Ce travail a montré que le routage sédimentaire du SE de la France actuel commence à s'établir dès l'Oligocène supérieur, avec la mise en place d'un système longitudinal (paléo-Rhône) pérenne dans la vallée du Rhône s'écoulant vers le Golfe du Lion et approvisionné par deux systèmes transverses (paléo-Isère & paléo-Durance) majeures assurant la connexion avec les Alpes de l'ouest. Dans le deuxième volet, des résultats de thermochronologie détritique confirment qu'à 30 Ma, une nouvelle source apparaît dans l'enregistrement sédimentaire des bassins rupéliens et dont l'origine est située dans le nord des Alpes internes. Cette source disparaît au Chattien dans le bassin d'avant pays ouest alpin, remplacée par une source des zones internes du sud, en lien avec l'exhumation des Alpes externes causant une migration de la ligne de partage des eaux et une réorganisation du réseau de drainage. Le Miocène est caractérisé par des apports permanents en provenance des Alpes internes bien que la sédimentation au cours de cette période soit fortement influencée par l'exhumation des Alpes externes. Nos résultats ont montré que le socle des Alpes externes devient une source au Tortonien. Dans le troisième volet, nous montrons que les flux sédimentaires chutent à l'Aquitanien moyen, jusqu'au Burdigalien supérieur, fait commun à l'ensemble du bassin d'avant pays pro foreland, et que nous avons relié à une diminution des apports lié à une réorganisation du réseau de drainage en lien avec l'exhumation des Alpes externes. Le début du Langhien est caractérisé par une augmentation très rapide des volumes sédimentés, les taux volumiques resteront très hauts jusqu'au Tortonien inférieur. Nous avons relié cette augmentation a deux causes : une réadaption du réseau de drainage et le recyclage du bassin d'avant pays nord alpin dans le bassin d'avant pays ouest alpin. La fin du Miocène est caractérisée par de très faibles volumes sédimentés, impliquant que le bassin d'avant pays ouest alpin est devenu une zone de transfert sédimentaire et que l'essentiel du matériel alpin est désormais exporté vers le Golfe du Lion. L'ensemble des résultats acquis nous a permis de proposer un modèle d'évolution paléoenvironnementale et source to sink du bassin d'avant pays ouest alpin composé de six phases entre l'Eocène et le Miocène supérieur, correspondant chacune à des changements majeurs dans l'enregistrement sédimentaire
The formation of the West Alpine foreland Basin results from the alpine collision starting from ~34 Ma and the exhumation of the internal Alps during the Oligocene and the external Alps during the Miocene. Its development is divided into two distinct phases: an underfilled basin between the Eocene and the middle Rupelian and an overfilled basin from the upper Rupelian until the end of the Miocene. The evolution of the sedimentation and the source to sink framework during this second phase are still poorly documented. The aim of this work is to provide new data and a better understanding of the development of this basin. This manuscript consists of three main parts. The first part focuses on the reorganization of sediment routing between the Eocene and the lower Miocene. For the first time, a precise and detailed chronostratigraphic synthesis of all Oligocene basins in southeastern France is proposed through the acquisition of new field and biostratigraphic data, as well as the reinterpretation of subsurface data. This work has highlighted the crucial role of the Pyrenean-Provencal orogeny, which promotes the export of Alpine material outside the foredeep from the upper Rupelian and the ECRIS, which creates subsiding zones in the Rhone Valley from the Priabonian, influencing the rest of Oligo-Miocene sedimentation. The development of the orogenic wedge and the exhumation of the external Alps caused, particularly during the Chattian, a decrease in sedimentary inputs from the internal Alps into the Oligocene basins. This work has shown that the current sediment routing in southeastern France began to establish itself from the upper Oligocene, with the establishment of a long-lasting longitudinal system (paleo-Rhone) in the Rhone Valley flowing towards the Gulf of Lion and fed by two major transverse systems (paleo-Isere & paleo-Durance) ensuring connection with the western Alps. In the second part, detrital thermochronology results confirm that at 30 Ma, a new source appears in the sedimentary record of the Rupelian basins, originating from the northern internal Alps. This source almost disappears during the Chattian in the West Alpine Foreland Basin, replaced by a source from the internal zones of the south, related to the exhumation of the external Alps causing a migration of the drainage divide and a reorganization of the drainage network. The Miocene is characterized by continuous inputs from the internal Alps although sedimentation during this period is strongly influenced by the exhumation of the external Alps. Our results have shown that the basement of the external Alps becomes a source in the Tortonian. In the third part, we show that sediment fluxes decrease in the middle Aquitanian, up to the upper Burdigalian, a phenomenon common to the entire foreland basin, which we have linked to a decrease in sedimentary inputs associated with a reorganization of the drainage network related to the exhumation of the external Alps. The beginning of the Langhian is characterized by a very rapid increase in sediment volumes, with volumetric rates remaining very high until the lower Tortonian. We have linked this increase to two causes: a readjustment of the drainage network and the recycling of sediment from the northern Alpine foreland basin into the western Alpine foreland basin. The end of the Miocene is characterized by very low sediment volumes, implying that the West Alpine Foreland Basin has become a sediment transfer zone and that most Alpine material is now exported to the Gulf of Lion. Based on our results, we propose a palaeoenvironmental and source to sink reconstruction for the West Alpine Foreland Basin, comprising six phases between the Eocene and Upper Miocene, each corresponding to major changes in the sedimentary record

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Pippèrr, Martina. "Early Miocene foraminifers from the Upper Marine Molasse of the North Alpine Foreland Basin – Proxies for biostratigraphy and palaeoenvironmental change". Diss., lmu, 2011. http://nbn-resolving.de/urn:nbn:de:bvb:19-127852.

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6

Mraz, Elena [Verfasser], Kurosch [Akademischer Betreuer] Thuro, Inga [Gutachter] Moeck, Thomas [Gutachter] Hamacher e Kurosch [Gutachter] Thuro. "Reservoir characterization to improve exploration concepts of the Upper Jurassic in the southern Bavarian Molasse Basin / Elena Mraz ; Gutachter: Inga Moeck, Thomas Hamacher, Kurosch Thuro ; Betreuer: Kurosch Thuro". München : Universitätsbibliothek der TU München, 2019. http://d-nb.info/1186256680/34.

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7

Symank, Ann-Isabelle [Verfasser], Michael [Gutachter] Alber e Wolfgang [Gutachter] Friederich. "The use of seismic attributes to increase the reliability of geothermal prospects in the South German Molasse Basin : the case study Kirchweidach / Ann-Isabelle Symank ; Gutachter: Michael Alber, Wolfgang Friederich ; Fakultät für Geowissenschaften". Bochum : Ruhr-Universität Bochum, 2019. http://d-nb.info/1204258252/34.

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8

Buoncristiani, Jean-François. "Production sédimentaire détritique des systèmes glaciaires. Quantification des produits stockés dans un lac proglaciaire durant la dernière glaciation : exemple du lac de la Combe d’Ain (Jura, France)". Dijon, 1997. http://www.theses.fr/1997DIJOS062.

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Cette thèse représente la quantification de la production sédimentaire détritique des systèmes glaciaires. L'objectif a été réalisé par l'étude d'un géosystème lacustre proglaciaire : le lac de la Combe d’Ain Jura, France). Le premier chapitre est consacré à l'analyse des différents processus d'érosion glaciaire actuels de façon qualitative et quantitative. Le chapitre 2 consiste à déterminer la surface du sous-système émetteur. Dans une première phase, le bassin-producteur supra-glaciaire est déterminé en fonction de la topographie de la surface glaciaire et des lignes d'écoulement. Puis, une seconde phase consiste à limiter le bassin sous-glaciaire en fonction de la topographie du substrat et de ses vallées. Dans le chapitre 3, l'organisation sédimentaire du sous-système récepteur est réalisé, ce qui permet de déterminer sa durée de fonctionnement. Le chapitre 4 représente la reconstruction de la géométrie des surfaces supérieures et inférieures du remplissage lacustre. Deux méthodes sont utilisées : une méthode directe (cartographie des témoins dans le remplissage), et une méthode géophysique indirecte (sismique réflexion haute résolution). Le chapitre 5 définit le bilan sédimentaire du géosysteme et permet le calcul des taux de stockage, puis des taux de production sédimentaire spécifique et de dénudation du géosysteme. Une comparaison avec le géosysteme lacustre de Chaillexon situé dans le jura et fonctionnant depuis 12 000 ans permet de définir les variations de la production sédimentaire au cours du dernier cycle climatique glaciaire-interglaciaire. On constate ainsi que la production sédimentaire durant la phase glaciaire est 100 fois supérieure a celle durant la phase interglaciaire. Il ressort de cette thèse la notion de rushes détritiques d'origine glaciaire, dont l'importance sur les exportations de matière dans les couloirs alluviaux et au-delà, sur les dépôts en domaine marin est à prendre en compte dans les bilans.

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9

Couëffé, Renaud. "La préservation du temps dans les enregistrements sédimentaires : analyse quantitative à l'intérieur de la molasse marine miocène du bassin d'avant-chaîne de Digne (Alpes de Haute Provence, sud-est de la France)". Caen, 2003. http://www.theses.fr/2003CAEN2022.

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Une nouvelle approche de la Molasse Marine miocène du bassin d'avant-chaîne de Digne est proposée à travers l'analyse quantitative du temps préservé dans l'enregistrement sédimentaire. L'étude détaillée des dépôts permet d'évaluer des taux de sédimentation utilisés pour quantifier le temps préservé à l'intérieur de séquences de dépôt d'une durée de 100 000 ans. Dans la majorité des cas, la part de temps préservé est très faible et les hiatus représentent l'essentiel du temps tandis que, dans certaines séquences, la forte proportion de temps préservé souligne le caractère beaucoup plus complet de l'enregistrement sédimentaire. Les paramètres évoqués pour rendre compte de cette forte variabilité du temps préservé sont la dynamique sédimentaire et l'accommodation. La démarche développée dans ce travail permet, à travers l'analyse du temps préservé dans l'enregistrement sédimentaire de la Molasse Marine, de proposer une méthode originale d'identification des processus d'accommodation.

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10

Largois, PHILIPPE. "La molasse miocene du bassin de digne (alpes de haute-provence) : interpretation paleoecologique des facies marins". Université Louis Pasteur (Strasbourg) (1971-2008), 2000. http://www.theses.fr/2000STR13228.

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L'etude de la molasse marine miocene de digne (alpes de haute-provence) est basee sur l'analyse ecosequentielle de la coupe de tanaron. A partir des donnees faunistiques (biofacies) et lithologiques (lithofacies) de tous les niveaux, le concept d'ecofacies a ete defini. Les ecofacies apparaissent comme des equivalents fossiles des ecosystemes benthiques actuels, notamment aux biocenoses en mer mediterranee (telles celles des sables fins bien calibres ; des vases terrigenes cotieres ; des fonds detritiques envases ; des sables grossiers et fins graviers sous l'influence de courants de fonds). Les donnees sedimentologiques et paleontologiques attestent de depots infralittoraux a circalittoraux (0 a 100 m). L'interpretation des ecosequences et de leur succession, auxquelles s'ajoutent les datations (87sr/86sr), confirment les sequences definies recemment a l'echelle des bassins europeens : les deux principales sequences correspondent aux deux premieres sequences burdigaliennes bur 1 et bur 2 (cycles de 3e ordre) ; elle s'etalent sur 2 ma - entre 20,52 (debut de la transgression burdigalienne) et 18,5 ma bp. Le sommet de la coupe marque le debut du cycle bur 3. Les ecosequences, de l'ordre de quelques metres pour atteindre exceptionnellement 10 a 20 m, sont progradantes ou retrogradantes, revelant des fluctuations bathymetriques relativement importantes. L'interpretation ecosequentielle fine a ete effectuee en etroite relation avec les ecofacies et les ecosystemes actuels, ce qui a permis d'envisager les correlations des ecofacies a l'echelle d'un bassin sedimentaire.

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Livros sobre o assunto "Molasse basin"

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Morend, Didier. High-resolution seismic facies of alluvial depositional systems in the Lower Freshwater Molasse (Oligocene-early Miocene, western Swiss Molasse Basin). Genève: Section des Sciences de la Terre, Université de Genève, 2000.

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2

Zweigel, J., Hans Fuchtbauer e A. P. Lisitzyn. Contributions to Sedimentology No. 20: Eustatic Versus Tectonic Control on Foreland Basin Fill, Sequence Stratigraphy, Subsidence Analysis, Stratigraphic Modelling, and Reservoir Modelling Applied to German Molasse Basin. Schweizerbartsche Verlagsbuchhandlung, E., 1998.

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3

Sommaruga, Anna. Geology of the Central Jura and the Molasse Basin: New Insight Into an Evaporite-Based Foreland Fold and Thrust Belt. Societe Neuchateloise des Sciences Naturelles, 1996.

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Capítulos de livros sobre o assunto "Molasse basin"

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Freeden, Willi, e Helga Nutz. "Test reservoir modeling in Bavarian molasse basin". In Exploratory Potential Methods in Geothermal Power Generation, 87–115. Cham: Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-54412-5_6.

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Hirner, Alfred V. "Metals in Crude Oils, Asphaltenes, Bitumen, and Kerogen in Molasse Basin, Southern Germany". In ACS Symposium Series, 146–53. Washington, DC: American Chemical Society, 1987. http://dx.doi.org/10.1021/bk-1987-0344.ch009.

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3

Deville, E., E. Blanc, M. Tardy, C. Beck, M. Cousin e G. Ménard. "Thrust Propagation and Syntectonic Sedimentation in the Savoy Tertiary Molasse Basin (Alpine Foreland)". In Hydrocarbon and Petroleum Geology of France, 269–80. Berlin, Heidelberg: Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-642-78849-9_19.

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4

Potten, Martin, Bettina Sellmeier, Elena Mraz e Kurosch Thuro. "Geomechanical Investigation of High Priority Geothermal Strata in the Molasse Basin, Bavaria, Germany". In IAEG/AEG Annual Meeting Proceedings, San Francisco, California, 2018 - Volume 2, 21–26. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-93127-2_4.

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5

Pfiffner, O. A., P. F. Erard e M. Stäuble. "Two cross sections through the Swiss Molasse Basin (lines E4–E6, W1, W7–W10)". In Deep Structure of the Swiss Alps, 64–72. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9098-4_8.

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Bieg, Ulrich, Michael Peter Süss e Joachim Kuhlemann. "Simulation of Tidal Flow and Circulation Patterns in the Early Miocene (Upper Marine Molasse) of the Alpine Foreland Basin". In Analogue and Numerical Modelling of Sedimentary Systems: From Understanding to Prediction, 145–69. Oxford, UK: Wiley-Blackwell, 2009. http://dx.doi.org/10.1002/9781444303131.ch6.

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Varghese, George. "Management of Impacted Third Molars". In Oral and Maxillofacial Surgery for the Clinician, 299–328. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-15-1346-6_14.

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AbstractThird molar impactions is one of the commonest minor oral surgical procedures in the realm of the oral and maxillofacial surgeon. Many basic principles of minor oral surgery have to be applied in a logical manner to attain a good healing. The assessment, clinical and radiographic evaluation plays an important role in selecting the right technique to ensure good results. This chapter aims to go through the basics of third molar impactions in a sequential way to guide the clinician to take the right decisions.

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Mamedov, Elkhan A. "Prediction and a new Method of Exploitation of Gold Deposits with Uranium in the Variscian Molass Conglomerate Basins of Germany". In Uranium, Mining and Hydrogeology, 67–68. Berlin, Heidelberg: Springer Berlin Heidelberg, 2008. http://dx.doi.org/10.1007/978-3-540-87746-2_9.

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Skinner, Matthew M., Philipp Gunz, Bernard A. Wood e Jean-Jacques Hublin. "How Many Landmarks? Assessing the Classification Accuracy of Pan Lower Molars Using a Geometric Morphometric Analysis of the Occlusal Basin as Seen at the Enamel-Dentine Junction". In Frontiers of Oral Biology, 23–29. Basel: KARGER, 2009. http://dx.doi.org/10.1159/000242385.

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"Molasse Basin". In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik, 886. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_132562.

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Trabalhos de conferências sobre o assunto "Molasse basin"

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H. Bachmann, G., e M. Muller. "Petroleum geology of the German Molasse Basin". In 56th EAEG Meeting. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609.201410138.

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Bechtel, A., M. Berling, P. David, F. Dax, T. U. Garlichs, R. Gratzer, D. Groß et al. "Oil-Source Correlation in the German Molasse Basin". In 29th International Meeting on Organic Geochemistry. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902720.

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Drews, M., W. Bauer e H. Stollhofen. "Reentering of an Overpressured Basin - The South German Molasse". In First EAGE Workshop on Pore Pressure Prediction. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201700049.

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Jin, J., T. Aigner e H. P. Luterbacher. "Seqeunce stratigraphy and depositional history in the Southeastern German Molasse Basin". In 56th EAEG Meeting. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609.201410217.

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Shipilin, V., H. von Hartmann, A. Friedrich e I. Moeck. "Constrained Migration Velocity Analysis - A Case Study in the German Molasse Basin". In 79th EAGE Conference and Exhibition 2017. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201701503.

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Gusterhuber, J., R. F. Sachsenhofer e H. G. Linzer. "A 2D Basin and Petroleum Systems Modelling Study in an Overthrust Setting - The Alpine Molasse Basin, Austria". In 73rd EAGE Conference and Exhibition incorporating SPE EUROPEC 2011. Netherlands: EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20149547.

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Büker, F., H. Horstmeyer e A. C. Green. "Shallow 3-D reflection seismic surveying of glacial sediments in the Swiss molasse basin". In 3rd EEGS Meeting. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609.201407282.

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Buker, F., A. Pugin, H. Horstmeyer e A. Green. "High-Resolution Seismic Mapping of Glacial and Proglacial Sediments in the Swiss Molasse Basin". In 1st EEGS Meeting. European Association of Geoscientists & Engineers, 1995. http://dx.doi.org/10.3997/2214-4609.201407434.

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von Hartmann, H. "Structure and Facies Analysis of a Carbonate Hydrogeothermal Reservoir within the Southern German Molasse Basin". In 71st EAGE Conference and Exhibition - Workshops and Fieldtrips. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609.201404962.

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Hinsch, R., e S. M. Hubbard. "Exploring for Stratigraphically Trapped Gas in Deep-Water Channel Deposits of the Austrian Molasse Basin". In 68th EAGE Conference and Exhibition incorporating SPE EUROPEC 2006. European Association of Geoscientists & Engineers, 2006. http://dx.doi.org/10.3997/2214-4609.201402050.

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Relatórios de organizações sobre o assunto "Molasse basin"

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GUSTERHUBER, Juergen, Reinhard F. SACHSENHOFER e Hans-Gert LINZER. A Multidimensional Basin and Petroleum Systems Modelling Study in an Overthrust Setting–the Alpine Molasse Basin, Austria. Cogeo@oeaw-giscience, setembro de 2011. http://dx.doi.org/10.5242/iamg.2011.0097.

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Turner, E. C. Mesoproterozoic Borden Basin, northern Baffin Island. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321825.

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The unmetamorphosed and nearly undeformed late Mesoproterozoic Borden Basin on northern Baffin Island exhibits sag, rift, and foreland-basin-like phases. A thin, partly subaqueous basal basalt is overlain by mature shallow-marine quartz arenite, upward-deepening siltstone and shale (marking the beginning of rifting), a complex suite of rift-delineated carbonate units containing two dramatic internal unconformities, and a flysch-molasse-like succession containing evidence of sediment derivation from the Grenville Orogen. Geochronological data indicate that deposition of most of the succession took place ca. 1100 to 1050 Ma. One of the carbonate intervals, Nanisivik Formation, is the main host of regional Zn-Pb showings including the past-producing Nanisivik orebody, which formed in the late Mesoproterozoic from low-temperature fluids, and which was emplaced under strong structural and stratigraphic controls. Minimal postdepositional deformation is limited to the emplacement of mafic dykes ca. 720 Ma and repeated reactivation of basement-rooted normal faults.

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