Sedimentary Environment of Pinghu Formation in Sudi Division,Xihu Ssg, the East China Sea
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Graphical Abstract
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Abstract
Sudi Division is located at the south part of center anticlinal zone. Pinghu Fm. of TWT Well 1 (1549.5m in thickness) have been interpreted by various views. This paper puts forward new points about depositional evolution based on depositional mechanism of transitional basin and stratum characteristics described by cyclostratigraphy.
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