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《Earth Science(Journal of China University of Geosciences)》 2009-05
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Late Oligocene Tectonic Event in the Northern South China Sea and Its Implications

SHAO Lei1,PANG Xiong2,ZHANG Gong-cheng3,QIAO Pei-jun1,LI Qian-yu1,WEI Gang-jian4,WU Meng-shuang2 1.State Key Laboratory of Marine Geology,Tongji University,Shanghai200092,China 2.CNOOC Ltd.,Shenzhen Branch,Guangzhou510240,China 3.Beijing Research Center of CNOOC Ltd.,Beijing100027,China 4.Guangzhou Institute of Geochemistry,CAS,Guangzhou510640,China  
A significant tectonic event was recorded in late Oligocene sediments from ODP Site 1148 and Pearl River Mouth Basin.This tectonic event coincided with the seafloor spreading axis jump event across the Oligocene/Miocene boundary,leading to a series of changes not only in seafloor spreading direction but also types of sedimentary basins and sediment provenances,and representing the greatest tectonic activity in the South China Sea region since the Oligocene.Sedimentation breaks and slumps as well as obvious changes in sediment composition across the Oligocene/Miocene boundary indicate the existence of the tectonic event,which transformed the Pearl River Mouth Basin from a graben basin to a down-warped basin,and the sedimentary environment in the Baiyun Sag area from continental shelf in the late Oligocene to continental slope since the early Miocene.It played a key role in the transformation of the general topographic character in continental China and ended a period of accumulation of good source rock for petroleum offshore.Therefore,this tectonic event has a profound influence on the evolution of the South China Sea and East Asia.
【Fund】: 国家重点研究专项经费(No.2007CB819501);; 国家科技重大专项(No.2008ZX05000-025);; 创新研究群体基金(No.40621063)
【CateGory Index】: P736.1
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