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《FAULT-BLOCK OIL & GAS FIELD》 1998-02
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On Terrigenous Sequence Boundary Model of the Steep Slope Zone in Fault-depressed Lacustrine Basin

Hu Shouquan (Petroleum Institute of Southwest, China)  
Because in the steep slope zone of fault-depressed lacustrine basin there is no sudden break which paleaotopography appears from gentle to steep, the depositional shoreline break is difficult to recognize. It has been put forward that the position of specific well is taken as reference to divide terrigenous sequence and system tract. The research result by using B207 as reference well shows that the three sequences of the upper member of Eh3 in researching area have 1 sequence boundary of type Ⅰ and 3 sequence boundaries of type Ⅱ. According to the thesis of four-division of system tract, a complete terrigenous sequence can be divided 4 system tracts and has 5 boundaries, of which the top and bottom belong to sequence boundary, and other 3 to system tract boundary, Parasequence boundary is a record of flooding in minor scale, and presents a flooding surface which is a transformation interface of sedimentary microfacies and the boundary which is equivalent to flooding surface.
【CateGory Index】: P539
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