s
  • 首页
  • 学报简介
  • 编委会
  • 投稿指南
  • 常见问题解答
  • 预出版
  • 过刊浏览
  • 联系我们
  • Engilsh

本文将参加年度优秀论文评选,如果您觉得这篇文章很好,请投下您宝贵的一票,谢谢! 支持(1)   不支持(0)

Development of the Miocene Guangle Carbonate Platform in the South China Sea: Architecture and Controlling Factors
投稿时间:2020-05-22  修订日期:2020-11-07  点此下载全文
引用本文:YANG Zhen,LI Xuelin,HUANG Lei,WANG Liaoliang,WU Shiguo,ZHANG Xinyuan.2021.Development of the Miocene Guangle Carbonate Platform in the South China Sea: Architecture and Controlling Factors[J].ACTA GEOLOGICA SINICA(English edition),95(1):177~191
摘要点击次数: 404
全文下载次数: 552
DOI:10.1111/1755-6724.14639
作者单位E-mail
YANG Zhen 1 Guangzhou Marine Geological Survey,China Geological Survey,Guangzhou 510075,China2 Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458,China  
LI Xuelin 1 Guangzhou Marine Geological Survey,China Geological Survey,Guangzhou 510075,China2 Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458,China3 Laboratory of Marine Geophysics and Georesource,Institute of Deep Sea Science and Engineering,Chinese Academy of Sciences,Sanya,Hainan 572000,China  
HUANG Lei 1 Guangzhou Marine Geological Survey,China Geological Survey,Guangzhou 510075,China2 Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458,China  
WANG Liaoliang 1 Guangzhou Marine Geological Survey,China Geological Survey,Guangzhou 510075,China2 Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458,China  
WU Shiguo 3 Laboratory of Marine Geophysics and Georesource,Institute of Deep Sea Science and Engineering,Chinese Academy of Sciences,Sanya,Hainan 572000,China4 Laboratory for Marine Geology,Qingdao National Laboratory for Marine Science and Technology,Qingdao,Shandong 266061,China swu@idsse.ac.cn 
ZHANG Xinyuan 4 Laboratory for Marine Geology,Qingdao National Laboratory for Marine Science and Technology,Qingdao,Shandong 266061,China  
 
Author NameAffiliationE-mail
YANG Zhen 1 Guangzhou Marine Geological Survey,China Geological Survey,Guangzhou 510075,China2 Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458,China  
LI Xuelin 1 Guangzhou Marine Geological Survey,China Geological Survey,Guangzhou 510075,China2 Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458,China3 Laboratory of Marine Geophysics and Georesource,Institute of Deep Sea Science and Engineering,Chinese Academy of Sciences,Sanya,Hainan 572000,China  
HUANG Lei 1 Guangzhou Marine Geological Survey,China Geological Survey,Guangzhou 510075,China2 Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458,China  
WANG Liaoliang 1 Guangzhou Marine Geological Survey,China Geological Survey,Guangzhou 510075,China2 Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458,China  
WU Shiguo 3 Laboratory of Marine Geophysics and Georesource,Institute of Deep Sea Science and Engineering,Chinese Academy of Sciences,Sanya,Hainan 572000,China4 Laboratory for Marine Geology,Qingdao National Laboratory for Marine Science and Technology,Qingdao,Shandong 266061,China swu@idsse.ac.cn 
ZHANG Xinyuan 4 Laboratory for Marine Geology,Qingdao National Laboratory for Marine Science and Technology,Qingdao,Shandong 266061,China  
Abstract:This study investigates the evolution of the Miocene Guangle carbonate platform (or Triton Horst) of the northwestern South China Sea margin.The platform is located at a junction area surrounded by Yinggehai basin,Qiongdongnan basin and Zhongjiannan basin.Well and regional geophysical data allow the identification of the morphologic and stratigraphic patterns.The Guangle carbonate platform was initiated on a tectonic uplift during the Early Miocene.The early platform was limited at Mesozoic granitic basement,pre-Paleogene sediments localized tectonic uplift and was small extension at the beginning stage.While during the Middle Miocene,the carbonate buildup flourished,and grow a thrived and thick carbonate succession overlining the whole Guangle Uplift.The isolated platforms then united afterward and covered an extensive area of several tens of thousands of square kilometers.However,it terminated in the Late Miocene.What are the control factors on the initiation, growth and demise of the Guangle carbonate platform? The onset of widespread carbonate deposits largely reflected the Early Miocene transgression linked with early post-rift subsidence and the opening of the South China Sea.Stressed carbonate growth conditions on the Guangle carbonate platform probably resulted from increased inorganic nutrient input derived from the adjacent uplifted mainland,possibly enhanced by deteriorated climatic conditions promoting platform drowning.Therefore, tectonics and terrigenous input could be two main controlling factors on the development of the Guangle carbonate platforms and main evolution stages.
keywords:carbonate platform,seismic characteristics,tectonic subsidence,South China Sea
查看全文  查看/发表评论  下载PDF阅读器
您是第92884726位访问者  京ICP备05032737号-7  京公网 安备110102004559
版权所有:Acta Geologica Sinica (English Edition)
主管单位:中国科学技术协会 主办单位:中国地质学会
地  址: 北京市阜成门外百万庄26号 邮编:100037 电话:010-68999024 E-mail: geoacta@163.com
本系统由北京勤云科技发展有限公司设计 

京公网安备 11010202007916号

WeChat