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《Progress in Geophysics》 2014-05
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Comparison of fault structure characteristics in the northern Pearl River Mouth Basin and its geological implication

CAO Jing-he;XIA Shao-hong;SUN Jin-long;XU Hui-long;Key Laboratory of Marginal Sea Geology,South China Sea Institute of Oceanology,Chinese Academy of Sciences;Graduate University of Chinese Academy of Science;  
Faults are the dominating factor generate a framework that belts in S-N and blocks in E-W in the Pearl River Mouth Basin(PMRB),which also has close relationship with hydrocarbon migration and the formation and distribution of reservoirs.Based on the multichannel seismic data in the northern PMRB and reflection seismic data collected in its adjacent sea area,this paper conducts a comparative research on fault structure characteristics in the interior and boundary of Northern Fault Terrace Zone(NFTZ),Northern Depression Zone(NDZ)and Central Uplift Zone(CUZ)of the northern PMRB.The results show that NFTZ mainly develops slabsurface faults which dip southeast.The faults are mostly developed in NDZ,which combine the styles of half graben,horst,and narrow graben.The antithetic shovel-like faults which dip northwest are widely developed in CUZ.The fault activity rate in the northern PMRB is the highest in faultedsubsidence stage,followed by depressed-subsidence stage,and thermal subsidence stage lowest.The distinction regarding fault structure characteristics in different geological units are close related to the multi-episode stretch and differential uplift and subsidence of blocks in the northern PMRB.
【Fund】: 国家自然科学基金项目(91028002 41222039 41006027 U093306)资助
【CateGory Index】: P618.13;P631.4
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