Evolutionary mass flow-megaturbidites in an interplate basin: Example of the north Pyrenean basin
作者： Robert Bourrouilh
DOI: 10.1007/BF02237986
关键词: Cretaceous 、 Flysch 、 Mesozoic 、 Petroleum geology 、 Geology 、 Paleontology 、 Clastic rock 、 Structural basin 、 Sedimentary rock 、 Conglomerate 、 Geotechnical Engineering and Engineering Geology 、 Earth and Planetary Sciences (miscellaneous) 、 Environmental Science (miscellaneous) 、 Oceanography
摘要: The Cretaceous north Pyrenean interplate basin developed in conjunction with the opening of Bay Biscay deposition large amounts carbonates on its margins. Major failures linear segments shelf and slope generated autosuspended mass flows; some these flows differentiated orevolved into megaturbidites that are up to 63 m thick 95 km long. A study evolutionary flow-megaturbidites also has application petroleum geology because it can help detail anatomy a related distribution sedimentary bodies paleoenvironments.
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