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- W2085136309 abstract "A study of seismic lines and well data from the region between the Isar and Inn rivers (SE Germany) indicates the presence of three main depositional cycles in the Molasse Basin: Upper Eocene-Chattian Sands, Upper Chattian Marls-Aquitanian Sandstone-Shale Series and Aquitanian Fish Shales-Upper Freshwater Molasse. The flexural subsidence caused by thrust loading has the greatest influence in increasing/reducing the accommodation space for the deposition, which controlled the displacement of the depositional axis in a N-S direction. However, eustatic sea-level changes, which caused the shoreline to shift in a W-E direction, have a strong impact on the stratigraphic development of this typical foreland basin." @default.
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- W2085136309 date "1995-01-01" @default.
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- W2085136309 title "Sequence stratigraphy and depositional history in the south-eastern German Molasse Basin" @default.
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- W2085136309 doi "https://doi.org/10.1016/0264-8172(95)98856-z" @default.
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