Relevant bibliographies by topics / Molasse basin

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Molasse basin'

Author: Grafiati
Published: 21 September 2024
Last updated: 27 July 2025

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Journal articles on the topic "Molasse basin"

1

Pashko, Pandeli. "Morave Mt Oligocene-Middle Miocene succession of Albanian-Thessalian Basin." Bulletin of the Geological Society of Greece 52, no. 1 (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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Akgiin, Funda, and Hasan Sözbilir. "A palynostratigraphic approach to the SW Anatolian molasse basin: Kale-Tavas molasse and Denizli molasse." Geodinamica Acta 14, no. 1-3 (2001): 71–93. http://dx.doi.org/10.1080/09853111.2001.11432436.

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Akgün, F. "A palynostratigraphic approach to the SW Anatolian molasse basin: Kale–Tavas molasse and Denizli molasse." Geodinamica Acta 14, no. 1-3 (2001): 71–93. http://dx.doi.org/10.1016/s0985-3111(00)01054-8.

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Mamengko, David Victor, Yoga B.Sendjadja, Budi Mulyana, et al. "Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara." Jurnal Geologi dan Sumberdaya Mineral 20, no. 1 (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 th
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Mamengko, David Victor, Yoga B.Sendjadja, Budi Mulyana, et al. "Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara." Jurnal Geologi dan Sumberdaya Mineral 20, no. 1 (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 th
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Mamengko, David Victor, Yoga B.Sendjadja, Budi Mulyana, et al. "Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara." Jurnal Geologi dan Sumberdaya Mineral 20, no. 1 (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 th
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Mamengko, David Victor, Yoga B.Sendjadja, Budi Mulyana, et al. "Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara." Jurnal Geologi dan Sumberdaya Mineral 20, no. 1 (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 th
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Garefalakis, Philippos, and 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, no. 6 (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 t
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Bachmann, G. H., M. Müller, and K. Weggen. "Evolution of the Molasse Basin (Germany, Switzerland)." Tectonophysics 137, no. 1-4 (1987): 77–92. http://dx.doi.org/10.1016/0040-1951(87)90315-5.

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Reinecker, John, Mark Tingay, Birgit Müller, and Oliver Heidbach. "Present-day stress orientation in the Molasse Basin." Tectonophysics 482, no. 1-4 (2010): 129–38. http://dx.doi.org/10.1016/j.tecto.2009.07.021.

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Dissertations / Theses on the topic "Molasse basin"

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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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Seithel, Robin Jonas [Verfasser], and 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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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.<br>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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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
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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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Mraz, Elena [Verfasser], Kurosch [Akademischer Betreuer] Thuro, Inga [Gutachter] Moeck, Thomas [Gutachter] Hamacher, and 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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Symank, Ann-Isabelle [Verfasser], Michael [Gutachter] Alber, and 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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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
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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
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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). L
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Books on the topic "Molasse basin"

1

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

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Zweigel, J., Hans Fuchtbauer, and 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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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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Book chapters on the topic "Molasse basin"

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Freeden, Willi, and Helga Nutz. "Test reservoir modeling in Bavarian molasse basin." In Exploratory Potential Methods in Geothermal Power Generation. 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. American Chemical Society, 1987. http://dx.doi.org/10.1021/bk-1987-0344.ch009.

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

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Potten, Martin, Bettina Sellmeier, Elena Mraz, and 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. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-93127-2_4.

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

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Bieg, Ulrich, Michael Peter Süss, and 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. 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. 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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Biffi, A., F. Ballo, M. Gobbi, and G. Mastinu. "A Moving Laboratory for Automotive Components Safety Testing (MoLAS)." In Lecture Notes in Mechanical Engineering. Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-70392-8_131.

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AbstractThe MoLAS is a moving laboratory able to fully characterize the tire behavior in the real working environment. The basic structure of the moving laboratory is represented by a semi-trailer. A rotating frame that supports the measuring system is used to set the camber level by using an electric actuator. An electric steering actuation system guarantees high output torque and high output power. A pneumatic actuator is used to apply the vertical load, allowing to generate a large range of vertical force up to SUVs values. A complex driveline including an internal combustion engine (ICE) c
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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. 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, and 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. KARGER, 2009. http://dx.doi.org/10.1159/000242385.

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Conference papers on the topic "Molasse basin"

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Bäßler, Ralph, Alicija Boduch, and Joana Sobetzki. "Corrosion Resistance of High-alloyed Materials in Flowing Artificial Geothermal Water." In CORROSION 2014. NACE International, 2014. https://doi.org/10.5006/c2014-3825.

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Abstract Since geothermal wells are a feasible energy source to replace fossil fuel supply, many technologies have been developed to take advantage of geothermal energy. Nevertheless, service conditions in geothermal facilities are due to the chemical composition of hydrothermal waters and temperatures, in many cases, extreme in terms of corrosion. Therefore, materials selection based on preliminary material qualification is essential to guarantee a secure and reliable operation of the facilities. This contribution deals with the evaluation of the corrosion behavior of different steels in flow
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H. Bachmann, G., and 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, 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, and H. Stollhofen. "Reentering of an Overpressured Basin - The South German Molasse." In First EAGE Workshop on Pore Pressure Prediction. EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201700049.

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Jin, J., T. Aigner, and 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, and I. Moeck. "Constrained Migration Velocity Analysis - A Case Study in the German Molasse Basin." In 79th EAGE Conference and Exhibition 2017. EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201701503.

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Gusterhuber, J., R. F. Sachsenhofer, and 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. EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20149547.

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Büker, F., H. Horstmeyer, and 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, and 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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Reports on the topic "Molasse basin"

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GUSTERHUBER, Juergen, Reinhard F. SACHSENHOFER, and Hans-Gert LINZER. A Multidimensional Basin and Petroleum Systems Modelling Study in an Overthrust Setting–the Alpine Molasse Basin, Austria. Cogeo@oeaw-giscience, 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 t
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