Forced Regression and Normal Regression Deposition of Basin with Continental Shelf Slopebreak: A case study on Zhujiang and Hanjiang Formations of Pearl River Mouth Basin
- Received Date: 1900-01-01
- Rev Recd Date: 1900-01-01
- Publish Date: 2009-12-10
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Key words:
- Pearl River Mouth Basin
Abstract: The question about the deposition and the corresponding systems tract in forced regression is always the domestic and foreign focal point of argument. Integrated with sequence stratigraphic depositional model which was established by Exxon Corporation, forced regression deposition was corresponded to the early lowstand systems tract and the late highstand systems tract,the normal regression deposition was corresponded to progradation depositions of late lowstand systems tract, early highstand systems tract. Taking Zhujiang and Hanjiang Formations of Pearl River Mouth Basin as an example, they can be divided into 7 thirdorder relative sealevel change cycles, corresponding to 7 thirdorder sequence. The relative sealevel change is the external influence of the accommodate space change. The progradation depositions of late highstand systems tract distribute above the shelf slopebreak. The lowstand fans distribute on and under the slope. The lowstand wedges distribute on and under the slopebreak zone. The progradation depositions of early highstand systems tract distribute above the slopebreak zone. They are all the favorable reservoirs.
Citation: | XIE Lihua. Forced Regression and Normal Regression Deposition of Basin with Continental Shelf Slopebreak: A case study on Zhujiang and Hanjiang Formations of Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1093-1100. |