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《Acta Sedimentologica Sinica》 2006-04
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Northern Continental Slope Palaeogeomorphology and Deep-water Fan System Response of Pearl River Since 13.8Ma,South China Sea

LIU Bao-jun~(1) YUAN Li-zhong~(1) SHEN Jun~(1) LIAN Shi-yong~(1) HE Min~(1) PANG Xiong~(1) SHU Yu~(1) PENG Da-jun~(2)(1.Shenzhen Corpration,CNOOC,Guangzhou 510240;2.Chengdu University of Technology,Chengdu 610059)  
Implied integrated sequence stratigraphy and geophysical method to analyze the 13.8Ma palaeogeomorphology of Baiyun sag,Pearl River Mouth Basin(PRMB).Submarine fan systems distribution,deposit characteristics and sequence stratigraphy filling evolvement analysis on sequence development from 13.8Ma implied that Baiyun sag lies in wide-slow continental shelf's slope area and develop two types canyons/channels on the north shelf margin,that Baiyun sag became to flat and open,and that submarine fan deposition are mainly controlled by palaeogeomorphology、sediment supply and fluctuation of climate.At the same time,north of South China Sea continental slope deepwater area's depositional topography has been similar characteristic from 13.8Ma to today,and today's submarine valley topography by and large implicated depositional paleo-geomorphology environment.It is concluded that deepwater deposition,which are mainly controlled by paleo-topography and evolvement rather than sea level changes,had been similar depositional topography character with today.
【Fund】: 全国油气资源战略选区调查及评价项目(XQ2004-05);; 国家自然科学基金重点项目(批准号:40238060)联合资助
【CateGory Index】: P531
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