Structural Variability and Rifting Process of the Segmented Cenozoic Pearl River Mouth Basin,Northern Continental Margin of the South China Sea  

作　　者：MA Bingshan QI Jiafu WU Guanghui REN Jianye YANG Linlong SUN Tong CHEN Shi CHEN Weichang GE Jiawang 

机构地区：[1]School of Geoscience and Technology,Southwest Petroleum University,Chengdu 610500,China [2]College of Geosciences,China University of Petroleum(Beijing),Beijing 102249,China [3]College of Marine Science and Technology,China University of Geosciences,Wuhan 430074,China [4]Working Station for Postdoctoral Scientific Research,Shengli Oilfield,Dongying,Shandong 257001,China [5]Research Institute of Petroleum Exploration,Dagang Oilfield Company,Tianjin 300450,China [6]College of Geography,Jining Normal University,Ulanqab,Inner Mongolia 012000,China

出　　处：《Acta Geologica Sinica(English Edition)》2022年第6期2074-2092,共19页地质学报（英文版）

基　　金：supported by the National Natural Science Foundation of China(Grant Nos.41572202 and 41902124).

摘　　要：The Pearl River Mouth Basin(PRMB)is an important area for studying the evolution of continental marginal basins in the northern South China Sea(SCS),but the structural variability and spatiotemporal rifting process remains poorly understood.This study investigates the differential structural features of the eastern,middle and western PRMB,as well as the extensional deformation laws in operation during the rifting stage,according to an integrated analysis of geometric characteristics and kinematic parameters,i.e.,horizontal displacement and stretching factors of basin and crust.The PRMB underwent at least three phases of intense extension,which varied in time and space.(1)During the middle Eocene,most sags in the PRMB were intensely stretched and high-angle planar to listric boundary faults controlled the wedge-shaped stratigraphic geometry.(2)During the late Eocene-to-early Oligocene,the stratigraphic geometry of the sags was slightly wedge-shaped and continuously controlled by boundary faults,however,the extensional strength decreased relatively in the Northern depression zone,but increased in the Southern depression zone.(3)During the late Oligocene,the extension was extremely weak in the northeast PRMB,but relatively strong in the southwest PRMB,leading to tabular stratigraphic geometry in the northeast PRMB,but localized slightly wedge-shaped stratigraphic geometry in the southwest.The southwest PRMB still underwent relatively strong extension during the early Miocene.The southwest PRMB that was induced by a small-scale localized mantle convection system constantly rifted during the late Oligocene,controlled by the weak lithosphere,westward(southwestward)diachronous opening and southward jump of the ocean ridge.The applied quantitative parameters and spatiotemporal rifting process may be used as a reference with which to study the segmented continental margin rifts.

关 键 词：basin structure extensional feature rifting process Pearl River Mouth Basin northern South China Sea 

分 类 号：P534.6[天文地球—古生物学与地层学] P542[天文地球—地质学]