The Role of Bottom Currents on the Morphological Development Around a Drowned Carbonate Platform,NW South China Sea  

作　　者：YU Kaiqi ALVES Tiago M LI Wei LI Shuang LI Jian ZHAO Fang WU Shiguo ZHAN Wenhuan 

机构地区：[1]CAS Key Laboratory of Ocean and Marginal Sea Geology,South China Sea Institute of Oceanology,Chinese Academyof Sciences,Guangzhou 510301,China [2]Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou),Guangzhou 511458,China [3]University of Chinese Academy of Sciences,Beijing 100049,China [4]3D Seismic Laboratory,School of Earth and Ocean Sciences,Cardiff University,Cardiff CF103AT,UK [5]Institute of Deep-Sea Science and Engineering,Chinese Academy of Sciences,Sanya 572000,China

出　　处：《Journal of Ocean University of China》2022年第4期801-812,共12页中国海洋大学学报（英文版）

基　　金：We thank the PetroChina Hangzhou Research Institute of Geology for the permissions to release the seismic data.This study was financially supported by the Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou)(No.GML2019ZD0104);the Guangdong Basic and Applied Basic Research Foundation(No.2020B1515020016);the National Natural Science Foundation of Guangdong Province(No.2020A1515010497);the National Natu-ral Science Foundation of China(No.41876054);the Guangdong Pearl River Talents Program(No.2017GC010510);Dr.Wei Li is specially funded by the CAS Pioneer Hundred Talents Program(No.Y8SL011001).

摘　　要：The seafloor around carbonate platforms is largely shaped and modified by downslope processes.However,the role of alongslope processes,including bottom currents,on the morphological development of carbonate platforms remains poorly understood.Here,we use high-resolution multibeam bathymetric data and two-dimensional seismic profiles to investigate the detailed sea-floor morphology around the Zhongjianbei carbonate platform(ZCP)in the northwest South China Sea.A series of depositional bodies and erosional channels are identified to the south of the ZCP and are interpreted as contourite drifts and channels resulted from the interaction between bottom currents and bathymetric features.In addition,active fluid seepages have led to the formation of widespread pockmarks on the seafloor.Importantly,the contourite channels and widespread pockmarks also show a close relationship in their distribution.We propose that the contourite channels around the ZCP are evolved from the coalescence of pockmarks under the persistent erosion of bottom currents.Based on the morphological analysis,we reconstruct the past bottom-current pathways around the ZCP that are parallel to the platform slopes and heading to the south.This study provides new insights into the formation of complex bathymetry and helps understanding how bottom currents and active fluid seepages can influence the morphological development around carbonate platforms.

关 键 词：carbonate platform seafloor morphology contourite channels bottom currents fluid seepages South China Sea 

分 类 号：P736[天文地球—海洋地质]