Permian sequence stratigraphy of slope facies in southern Guizhou and chronostratigraphic correlation |
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Authors: | SHI Xiaoying MEI Shilong SUN Yan |
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Institution: | China University of Geosciences,Beijing 100083,China |
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Abstract: | The Permian in slope facies area of southern Guizhou consists of 16 third order sequences, which can be grouped as four sequence
sets and further into two mesosequences. Most of them are delineated by conformable or submarine erosion surfaces, and well
controlled by conodont and fusulinid zones. Four important sea-level falls are recognized in the area, which occur respectively
at the basalSweetognathodus whitei zone, lowerS.aff.hanzhongensis zone, middleJinogondolella xuanhanensis zone and the basalClarkina yini zone. Among the recognized transgression events, three are regarded as the most significant. They occur respectively at the
basalNeogondolella exculptus zone, basalJinogondolella nankingensis zone and the lowerClarkina postbitteri zone, and are all accompanied by faunal turnovers. The key surfaces in sequences can be used to fine-tune the boundaries
of bio-chronozones, stages and series. |
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Keywords: | Permian sequence stratigraphy slope facies southern Guizhou correlation |
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