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《Fault-Block Oil & Gas Field》 2009-02
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Origin of salt rock and classification of stratigraphic sequence for the third section of Shahejie Formation in Dongpu Depression

Zhao Junfeng1,2 Ji Youliang1 Su Hui3 Li Xingxing2 (1.School of Ocean and Earth Science, Tongji University, Shanghai 200092, China; 2.Well Logging Company, Zhongyuan Petroleum Exploration Bureau, SINOPEC, Puyang 457001, China; 3.Research Institute of Exploration and Development, Zhongyuan Oilfield Company, SINOPEC, Puyang 457001, China)  
In the highstand period of the third section of Shahejie Formation in Dongpu Depression, dark grey and dark mudstone and a few gravity flow sandbodies were deposited. And salt rock, gypsum rock, lowstand deltas and fan deltas were developed in the lowstand period. As a result, deep lacustrine facies mudstone is interbeded with evaporite and lowstand sandstone in vertical. According to the core data, characteristics of sedimentary sequence of salt rock, palaeoclimate and palaeoenvironment of depositional stage, this paper indicates that the origin of salt rock is because of shallow water evaporation. The dark mudstone deposited in deep water was interbedded with the salt rock deposited in shallow water, which showed that the lacustrine level changed frequently during the sedimentation of the third section of Shahejie Formation. Based on the method of parasequences identification with the salt rhythm characteristics, the sequence division accords with the practice in salt formation in Dongpu Depression.
【Fund】: 国家973项目“中国叠合盆地层序地层学及构造古地理研究”(G1999043304)资助
【CateGory Index】: P618.13
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