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《Acta Sedimentologica Sinica》 2001-02
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Sequence Stratigraphy of Jurassic in Turpan-Hami Basin

SHEN Shou wen 1 PENG Da jun 2 YAN Qi bin 1 HUANG Xian lü 2 LI Zhi jun 3 1(Department of Exploration, Southwest Petroleum Institute, Nanchong, Sichuan 637001) 2(Department of Petroleum, Chengdu College of Technology, Chengdu 610059  
Fourteen sequence boundaries showing onlap or erosional truncation are recognized in the seismic sections of the Jurassic Turpan Hami basin.The two major boundaries (at the top and bottom of the Jurassic deposits)are regional unconformities extending beyond the basin.Three intermediate ones (between 3 re and 4 th section of Xishanyao Fm.Qikeai Fm.and Sanjianfeng Fm.and Kalaza Fm.and Qigu Fm.) are unconformities spaning most of the basin.The remaining nine sequence boundaries are local unconformities.The Jurassic sedimentary strata in Turpan Hami basin is a basin fill sequence (1 st order)including four tectonic sequences(2 nd order) and thirteen depositional sequences(3 rd order).The four tectonic sequences are bound with the four evolutionary stages(stable subsidence,short time contraction,expansion,and uplift desiccation)of the lake basin. According to classic sequence stratigraphy,there are two types of sequences and sequence boundaries in passive continental margins with a shelf and slope.The types of depositional sequences in terrestrial basin,however,are not the same as those from a passive continental margin.Four types of sequence boundaries(type A,B,C,and D)are identified in the basin.A type A boundary is formed at the desiccation stage of the lake basin caused by strong tectonic uplift.The sequence above the type A boundary is here termed as fluvial sequence, in which the major systems tract is a lowstand deposit composed of alluvial fan and fluvial facies.A type B boundary,where base level falls below the previous shore slope break and then rises rapidly,occurs as the stage of basin expansion caused by rapid tectonic subsidence.The corresponding sequence without the lowstand systems tract is here termed as submerged sequence. A type C boundary,where base level also falls below the previous shore slope break and fluvial incision occurs,is similar to the type 1 boundary identified by Vail et al(1977).The lowstand systems tract with deposits of basin floor fan and incised valley overlies type C boundary.Therefore,type C sequence is called as similar type 1sequence . A type D boundary,where base level falls but shore slope is not exposed,is similar to type 2 boundary identified by Vail et al(1977).The corresponding sequence without the lowstand systems tract is here termed as similar type 2sequence. The difference between these boundary types is the nature of transgression above the boundary for type B and D.which both lack a lowstand systems tract.There is a gradual transgression in type D compared with a rapid and abrupt one in type B.In other words.the sedimentary facies above the type B boundary are distinct from those below the boundary and record a rapid change in base level compared with a gradual one in type D. Four types of sequence models in this paper have demonstrated the difference between marine facies sequences and non marine facies sequences.The type A boundary fluvial sequence and type B boundary submerged sequence are indicative of two extreme conditions of desiccation and rapid subsidence of the lake basin,and are totally different from marine facies sequences.We suggest several reasons for the variety of non marine facies sequences of the lake basin: a smaller scale,multiple sediment input provenances,relative short distance from sediment source.and differences in local tectonic activity. There is a relationship between the sequence stratigraphy and the hydrocarbon shows in well TC2 of Turpan Hami basin.Hydrocarbon shows are often adjacent to sequence boundaries in Kalaza Fm.and Qigu Fm.because both formations lack oil source rocks or/and source rocks are not at the depth of the oil window.Hydrocarbons originating from underlying formations thas migrate through fractures occur along the sequence boundaries.which usually have higher permeability.However.hydrocatbon shows in the Qiketai,Sanjianfeng,and Xishanyao formations are different from the overlying formations because they contain good source rocks buried to the oil window.In some for
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