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zhu jiang kou wai di si ji chen ji xiang de chu bu hua fen
Author(s): 
Pages: 371-380
Year: Issue:  4
Journal: Oil & Gas Geology

Keyword:  珠江口外沉积相第四纪海平面变化高分辨率地震;
Abstract: According to high resolution geophysical data inthe 3.5 kHz subbottom profile andsingle-channel seismic reflection,the Quaternary in the Pearl River mouth shelf can be di-vided into four main sedimentary facies and one special deposit body:fluvial facies,deltaicfacies,shallow sea facies,tidal current-bayou facies and sand dune-sand wave deposits.These different sedimentary facies are sedimentary systems that formed in low waterlevel,high water level of different periods and transgressive or regressive conditions con-trolled by regional eustasy during Pleistocene-Holocene.
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