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Journal articles on the topic 'Molasse basin'

Author: Grafiati

Published: 21 September 2024

Last updated: 27 July 2025

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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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2

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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3

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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4

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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6

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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7

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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8

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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9

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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10

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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11

Seithel, Robin, Emmanuel Gaucher, Birgit Mueller, Ulrich Steiner, and Thomas Kohl. "Probability of fault reactivation in the Bavarian Molasse Basin." Geothermics 82 (November 2019): 81–90. http://dx.doi.org/10.1016/j.geothermics.2019.06.004.

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12

Dostal, J., W. U. Mueller, and J. B. Murphy. "Archean Molasse Basin Evolution and Magmatism, Wabigoon Subprovince, Canada." Journal of Geology 112, no. 4 (2004): 435–54. http://dx.doi.org/10.1086/421073.

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13

Rühaak, Wolfram, Volker Rath, and Christoph Clauser. "Detecting thermal anomalies within the Molasse Basin, southern Germany." Hydrogeology Journal 18, no. 8 (2010): 1897–915. http://dx.doi.org/10.1007/s10040-010-0676-z.

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14

Garefalakis, Philippos, Fritz Schlunegger, Ariel Henrique Do Prado, David Mair, and Alexander C. Whittaker. "Constant size and mobility of grains in the Oligo-Miocene megafan deposits in the Swiss Molasse Basin despite long-term changes in tectonic processes, climatic conditions, and sediment flux." Journal of Sedimentary Research 95, no. 3 (2025): 507–31. https://doi.org/10.2110/jsr.2024.058.

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ABSTRACT The Swiss Molasse Basin, situated north of the Central European Alps, documents the tectono-geomorphological evolution of the foreland basin and the adjacent mountain belt. Tectonic perturbations in the Alpine source area, shifts in climatic conditions, or a combined effect thereof were reported to have been reflected by changes in the volumes of material supplied to the foreland basin. A frequently used signal to infer such geodynamic changes is the size of grains deposited on alluvial fans, preserved as conglomerate beds forming several hundreds of meters thick sections. Accordingly

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15

Rössner, Gertrud E. "A community of Middle Miocene Ruminantia (Mammalia, Artiodactyla) from the German Molasse Basin." Palaeontographica Abteilung A 277, no. 1-6 (2006): 103–12. http://dx.doi.org/10.1127/pala/277/2006/103.

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16

Meller, Barbara. "Wetland vegetation types in the Late Miocene Alpine Molasse Basin in Upper Austria." Palaeontographica Abteilung B 287, no. 1-6 (2011): 57–155. http://dx.doi.org/10.1127/palb/287/2011/57.

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17

Maurer, Holger, and Elmar Buchner. "Fluvial systems of the Upper Freshwater Molasse (North Alpine Foreland Basin, SW-Germany)." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 158, no. 2 (2007): 249–70. http://dx.doi.org/10.1127/1860-1804/2007/0158-0249.

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18

Becker, Damien, Pierre-Olivier Antoine, Burkart Engesser, et al. "Late Aquitanian mammals from Engehalde (Molasse Basin, Canton Bern, Switzerland)." Annales de Paléontologie 96, no. 3 (2010): 95–116. http://dx.doi.org/10.1016/j.annpal.2011.03.001.

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19

Jodocy, Marco, and Ingrid Stober. "Geologic-geothermal cross-sections through the southwestern part of the Molasse Basin (South Germany)." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 160, no. 4 (2009): 359–66. http://dx.doi.org/10.1127/1860-1804/2009/0160-0359.

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20

Meszar, Maria, Susanne Gier, Markus Palzer-Khomenko, Wolfgang Knierzinger, and Michael Wagreich. "Clay mineralogy of Miocene mudstones from the Lower Austrian Molasse Basin." Austrian Journal of Earth Sciences 113, no. 1 (2020): 125–38. http://dx.doi.org/10.17738/ajes.2020.0008.

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Abstract Recent studies established the lithological and chemical sediment evolution in the Lower Austrian Molasse Basin (LAMB), a part of the North Alpine foreland basin, during the Early Miocene. In this study, we aim to integrate the clay mineralogy of seven wells across the LAMB with a newly proposed lithostratigraphy, and to infer implications for provenance, palaeo-geography and palaeoclimate. The results of our qualitative and quantitative evaluation of the clay-sized fraction with x-ray diffractometry largely support the stratigraphic model. The early stage of foreland basin formation

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21

Rybach, Ladislaus. "Geothermal potential of Sedimentary Basins, especially of the Swiss Molasse Basin." Földtani Közlöny 149, no. 4 (2019): 401. http://dx.doi.org/10.23928/foldt.kozl.2019.149.4.401.

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Sedimentary basins usually have significant geothermal potential. Deep aquifers are key components. The factors, conditions, and processes that define and control the potential are: processes during basin formation like sedimentation, karstification, fracturing; rock porosity, permeability/fluid content; depth/temperature; hydrogeology; production sustainability. They are demonstrated on selected examples: USA basins, Paris Basin, Molasse Basin. Of the latter, the French, German and Austrian parts are treated first and then the Swiss Molasse Basin (SMB) in more detail.The various efforts under

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22

Gier, S. "Clay mineral and organic diagenesis of the Lower Oligocene Schöneck Fishshale, western Austrian Molasse Basin." Clay Minerals 35, no. 4 (2000): 709–17. http://dx.doi.org/10.1180/000985500547151.

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AbstractThe ‘Fischschiefer formation’ has been identified as the likely source rock for petroleum in the western Molasse Basin of Austria. The investigated cores originate from different depths (1242 m to 4294 m) of the Fischschiefer horizon. The illitization observed in the <0.2 μm fraction proceeds slowly, probably because of the low geothermal gradient (3°C/100 m) in the Molasse Basin. The illite content in illite-smectite ranges from 30% (randomly ordered) for the shallowest sample to 65% (R0+R1 ordering) for the deepest sample. The oxygen index (OI) vs. hydrogen index (HI) plot implies

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23

Heine, Florian, Kai Zosseder, and Florian Einsiedl. "Hydrochemical Zoning and Chemical Evolution of the Deep Upper Jurassic Thermal Groundwater Reservoir Using Water Chemical and Environmental Isotope Data." Water 13, no. 9 (2021): 1162. http://dx.doi.org/10.3390/w13091162.

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A comprehensive hydrogeological understanding of the deep Upper Jurassic carbonate aquifer, which represents an important geothermal reservoir in the South German Molasse Basin (SGMB), is crucial for improved and sustainable groundwater resource management. Water chemical data and environmental isotope analyses of δD, δ18O and 87Sr/86Sr were obtained from groundwater of 24 deep Upper Jurassic geothermal wells and coupled with a few analyses of noble gases (3He/4He, 40Ar/36Ar) and noble gas infiltration temperatures. Hierarchical cluster analysis revealed three major water types and allowed a h

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24

Schumacher, S., and R. Schulz. "Effectiveness of acidizing geothermal wells in the South German Molasse Basin." Geothermal Energy Science 1, no. 1 (2013): 1–11. http://dx.doi.org/10.5194/gtes-1-1-2013.

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<p><strong>Abstract.</strong> In Germany, many hydro-geothermal plants have been constructed in recent years, primarily in the region of Munich. As the host formation here mainly consists of carbonates, nearly all recently drilled wells have been acidized in order to improve the well yield. In this study, the effectiveness of these acid treatments is analyzed with respect to the amount of acid used and the number of acid treatments carried out per well. The results show that the first acid treatment has the largest effect, while subsequent acidizing improves the well only mar

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25

Chelle-Michou, Cyril, Damien Do Couto, Andrea Moscariello, Philippe Renard, and Elme Rusillon. "Geothermal state of the deep Western Alpine Molasse Basin, France-Switzerland." Geothermics 67 (May 2017): 48–65. http://dx.doi.org/10.1016/j.geothermics.2017.01.004.

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26

Schlunegger, Fritz, and Jon Mosar. "The last erosional stage of the Molasse Basin and the Alps." International Journal of Earth Sciences 100, no. 5 (2010): 1147–62. http://dx.doi.org/10.1007/s00531-010-0607-1.

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27

Gjoka, Michail, and Alekssander Dulaj. "Overpressuring in the molasse deposits of the Adriatic Basin in Albania." Petroleum Geoscience 3, no. 3 (1997): 259–68. http://dx.doi.org/10.1144/petgeo.3.3.259.

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28

Shalaby, A., K. Stüwe, H. Fritz, and F. Makroum. "The El Mayah molasse basin in the Eastern Desert of Egypt." Journal of African Earth Sciences 45, no. 1 (2006): 1–15. http://dx.doi.org/10.1016/j.jafrearsci.2006.01.004.

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29

Friend, P. F. "Molasse basins of Europe: a tectonic assessment." Transactions of the Royal Society of Edinburgh: Earth Sciences 76, no. 4 (1985): 451–62. http://dx.doi.org/10.1017/s0263593300010658.

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ABSTRACTSedimentary basins are structures that formed either by subsidence of an area relative to its surroundings, or by uplift of the surroundings. The basin is defined by its sedimentary fill, and the vertical kinematics of the fill are reflected by stratal wedging, unconformities and, or, faulting. The following basin mechanisms are distinguished: locally (a) stretch, (b) thrust and piggy-back, (c) local uplift, and regionally (d) stretch-and-cool, (e) load-and-flex and (f) cratonic uplift.Basin patterns are reviewed for the three main Phanerozoic episodes for which molasse-like features o

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30

Mödden, Clemens. "Biostratigraphic correlations in the lowermost Miocene of the Mainz Basin and the western Molasse Basin based on fossil mammals." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 202, no. 1 (1996): 111–16. http://dx.doi.org/10.1127/njgpa/202/1996/111.

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31

Haas, Maximilian, Davide Carraro, Dario Ventra, Michael Plötze, Haller Antoine De, and Andrea Moscariello. "Integrated stratigraphic, sedimentological and petrographical evaluation for CERN's Future Circular Collider subsurface infrastructure (Geneva Basin, Switzerland‑France)." Swiss Journal of Geosciences 115, no. 16 (2022): 43. https://doi.org/10.1186/s00015-022-00407-y.

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The European Organization for Nuclear Research (CERN) is currently undertaking a feasibility study to build the next generation particle accelerator, named the Future Circular Collider (FCC), hosted in a 90–100 km subsurface infrastructure in the Geneva Basin, extending across western Switzerland and adjacent France. This article represents a preliminary, basin-scale stratigraphic and lithotype analysis using state-of-the-art Swiss and French stratigraphic terminology, set in context with the FCC. Existing stratigraphic information, rock cores and well reports, laboratory analyses and ge

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32

Willett, Sean D., and Fritz Schlunegger. "The last phase of deposition in the Swiss Molasse Basin: from foredeep to negative-alpha basin." Basin Research 22, no. 5 (2010): 623–39. http://dx.doi.org/10.1111/j.1365-2117.2009.00435.x.

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33

Jost, Jürg, Daniel Kälin, Saskia Börner, Davit Vasilyan, Daniel Lawver, and Bettina Reichenbacher. "Vertebrate microfossils from the Upper Freshwater Molasse in the Swiss Molasse Basin: Implications for the evolution of the North Alpine Foreland Basin during the Miocene Climate Optimum." Palaeogeography, Palaeoclimatology, Palaeoecology 426 (May 2015): 22–33. http://dx.doi.org/10.1016/j.palaeo.2015.02.028.

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34

Berger, Jean-Pierre. "Paleogeographic-palinspastic maps of the Swiss Molasse Basin (Early Oligocene-Middle Miocene)." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 202, no. 1 (1996): 1–44. http://dx.doi.org/10.1127/njgpa/202/1996/1.

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35

Krsnik, Emilija, Katharina Methner, Marion Campani, et al. "Miocene high elevation in the Central Alps." Solid Earth 12, no. 11 (2021): 2615–31. http://dx.doi.org/10.5194/se-12-2615-2021.

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Abstract. Reconstructing Oligocene–Miocene paleoelevation contributes to our understanding of the evolutionary history of the European Alps and sheds light on geodynamic and Earth surface processes involved in the development of Alpine topography. Despite being one of the most intensively explored mountain ranges worldwide, constraints on the elevation history of the European Alps remain scarce. Here we present stable and clumped isotope measurements to provide a new paleoelevation estimate for the mid-Miocene (∼14.5 Ma) European Central Alps. We apply stable isotope δ–δ paleoaltimetry to near

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36

Su, Wen, Shutong Xu, Laili Jiang, and Yican Liu. "Coesite from quartz-jadeitite in the Dabie Mountains, Eastern China." Mineralogical Magazine 60, no. 401 (1996): 659–62. http://dx.doi.org/10.1180/minmag.1996.060.401.12.

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The Dabie Mountains is a collisional orogen between the North China and Yantze Continental plates. It is composed, from south to north, of the foreland fold and thrust belt alternated with molasse basin, the subducted cover and basement of the Yangtze continental plate, the meta-ophiolitic melange belt, the forearc meta-flysch nappe (bounded by southward and northward thrust belts) in which there may be a buried volcanic arc and a relict back-arc basin (Fig. 1A) (Xu et al., 1992a, 1994).

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37

Jin, Jiuqiang, Thomas Aigner, H. P. Luterbacher, Gerhard H. Bachmann, and Manfred Müller. "Sequence stratigraphy and depositional history in the south-eastern German Molasse Basin." Marine and Petroleum Geology 12, no. 8 (1995): 929–40. http://dx.doi.org/10.1016/0264-8172(95)98856-z.

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38

Searle, M. P., K. T. Pickering, and D. J. W. Cooper. "Restoration and evolution of the intermontane Indus molasse basin, Ladakh Himalaya, India." Tectonophysics 174, no. 3-4 (1990): 301–14. http://dx.doi.org/10.1016/0040-1951(90)90327-5.

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39

Nebelsick, James H., Michael W. Rasser, and Ulrich Bieg. "The North Alpine Foreland Basin: Special Volume of the 2008 Molasse Meeting." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 254, no. 1 (2009): 1–4. http://dx.doi.org/10.1127/0077-7749/2009/0001.

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40

Schlunegger, Fritz, Dirk Rieke-Zapp, and Karl Ramseyer. "Possible environmental effects on the evolution of the Alps-Molasse Basin system." Swiss Journal of Geosciences 100, no. 3 (2007): 383–405. http://dx.doi.org/10.1007/s00015-007-1238-9.

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41

Andrews, J. N., M. J. Youngman, J. E. Goldbrunner, and W. G. Darling. "The geochemistry of formation waters in the molasse basin of upper Austria." Environmental Geology and Water Sciences 10, no. 1 (1987): 43–57. http://dx.doi.org/10.1007/bf02588004.

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42

Scholz, Herbert. "The conventional stratigraphical system of the Molasse used at the southern rim of the Molasse basin in southwestern Bavaria - proved or problematic?" Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 214, no. 3 (1999): 391–413. http://dx.doi.org/10.1127/njgpa/214/1999/391.

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43

Mennecart, Bastien, Bertrand Yerly, Pierre-Olivier Mojon, et al. "Postprint of Mennecart, B. et al. 2016. A new Late Agenian (MN2a, Early Miocene) fossil assemblage from Wallenried (Molasse Basin, Canton Fribourg, Switzerland). Paläontologische Zeitschrift 90, 101–123. doi:10.1007/s12542-015-0275-3." Paläontologische Zeitschrift 90, no. 1 (2016): 101–23. https://doi.org/10.1007/s12542-015-0275-3.

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Postprint of the publication: Mennecart, B., Yerly, B., Mojon, P.-O., Angelone, C., Maridet, O., Böhme, M., Pirkenseer, C., 2016. A new Late Agenian (MN2a, Early Miocene) fossil assemblage from Wallenried (Molasse Basin, Canton Fribourg, Switzerland). <em>Paläontologische Zeitschrift</em> 90, 101–123. https://doi.org/10.1007/s12542-015-0275-3

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44

Koch, Roman. "Upper Jurassic facies development in the subsurface of Lake Constance – Southern Germany; Molasse Basin. Where did the “Swabian Marl-Basin” disappear?" Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 101 (April 11, 2019): 359–93. http://dx.doi.org/10.1127/jmogv/101/0015.

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45

Schegg, Roland, Chris Cornford, and Werner Leu. "Migration and accumulation of hydrocarbons in the Swiss Molasse Basin: implications of a 2D basin modeling study." Marine and Petroleum Geology 16, no. 6 (1999): 511–31. http://dx.doi.org/10.1016/s0264-8172(99)00018-5.

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46

Ershov, Andrei V., Marie-Françoise Brunet, Maxim V. Korotaev, Anatoly M. Nikishin, and Sergei N. Bolotov. "Late Cenozoic burial history and dynamics of the Northern Caucasus molasse basin: implications for foreland basin modelling." Tectonophysics 313, no. 1-2 (1999): 219–41. http://dx.doi.org/10.1016/s0040-1951(99)00197-3.

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47

Schegg, Roland. "Coalification, shale diagenesis and thermal modelling in the Alpine Foreland basin: the Western Molasse basin (Switzerland/France)." Organic Geochemistry 18, no. 3 (1992): 289–300. http://dx.doi.org/10.1016/0146-6380(92)90070-e.

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48

SCHWARTZ, S., S. GUILLOT, P. TRICART, et al. "Source tracing of detrital serpentinite in the Oligocene molasse deposits from the western Alps (Barrême basin): implications for relief formation in the internal zone." Geological Magazine 149, no. 5 (2012): 841–56. http://dx.doi.org/10.1017/s0016756811001105.

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AbstractWe present the first contribution of tracing the source area of ophiolitic detritus in the Alpine molasse deposits by Raman spectroscopy. The lower Oligocene molasse deposits preserved in the Barrême basin, in the SW foreland of the western Alpine arc, are known for the sudden arrival of the first ‘exotic’ detritus coming from the internal Alpine zones. Among them, the pebbles of serpentinized peridotites have so far not been studied. We show that they only consist of antigorite serpentinite, implying that they originate from erosion of high temperature blueschists. In contrast, the up

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49

Aziz, Nabaz. "U-Pb ZIRCON DATING OF MIDDLE EOCENE CLASTIC ROCKS FROM THE GERCUS MOLASSE, NE IRAQ: NEW CONSTRAINTS ON THEIR PROVENANCE, AND TECTONIC EVOLUTION." Iraqi Geological Journal 54, no. 1C (2021): 1–15. http://dx.doi.org/10.46717/igj.54.1c.1ms-2021-03-21.

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The provenance of Middle Eocene clastic rock from the Gercus Molasse, NE Iraq was determined by detrital zircon (DZ) U-Pb geochronology. The Gercus Molasse in the Iraqi segment of the north-eastern Zagros Thrust Zone provides an ideal example of foreland system evolution with respect to the transition from passive margin to the accretionary complex terrene-flexural foreland basins. The DZ U-Pb age spectra from the Gercus Molasse suggest that the foreland sediments either influx from multiple provenances or are the result of recycling from the accretionary complex terrane. During pre-accretion,

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Singh, A. K., and J. N. Singh. "Sequence Stratigraphic Analysis of Pre-Tertiary Succession in Ganga Basin." Journal Geological Society of India 49, no. 6 (1997): 629–46. http://dx.doi.org/10.17491/jgsi/1997/490603.

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Abstract The paper defines the Pre-Tertiary stratigraphy of the Ganga Basin which is concealed beneath the thick cover of Cenozoic sediments. The sub-surface structural configuration is characterised by development of four major depressions, separated by transverse uplifts. Ganga Basin represents two main stages of geological evolution: a pre-collisional (Pre-Tertiary) stage consisting mainly of Proterozoic and Gondwana sediments, and a post-collisional (Tertiary) stage representing the Siwalik molasse. The Pre-Tertiary succession is classified into four mega sequences; three of these represen

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