Sequence stratigraphy and depositional history in the south-eastern German Molasse Basin

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 Fres...

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Bibliographic Details
Published in:Marine and petroleum geology Vol. 12; no. 8; pp. 929,IN3,937,IN9,939 - 936,IN8,938,IN14,940
Main Authors: Jin, Jiuqiang, Aigner, Thomas, Luterbacher, H.P., Bachmann, Gerhard H., Müller, Manfred
Format: Journal Article
Language:English
Published: Oxford Elsevier Ltd 1995
Elsevier Science
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Summary: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.
ISSN:0264-8172
1873-4073
DOI:10.1016/0264-8172(95)98856-Z