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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Published in: | Marine and petroleum geology Vol. 12; no. 8; pp. 929,IN3,937,IN9,939 - 936,IN8,938,IN14,940 |
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Main Authors: | , , , , |
Format: | Journal Article |
Language: | English |
Published: |
Oxford
Elsevier Ltd
1995
Elsevier Science |
Subjects: | |
Online Access: | Get full text |
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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. |
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ISSN: | 0264-8172 1873-4073 |
DOI: | 10.1016/0264-8172(95)98856-Z |