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南海华南陆缘中生界层序地层模式与海平面变化
引用本文:王嘹亮,许中杰,张莉,李飞,程日辉.南海华南陆缘中生界层序地层模式与海平面变化[J].世界地质,2010,29(3):431-441.
作者姓名:王嘹亮  许中杰  张莉  李飞  程日辉
作者单位:1. 广州海洋地质调查局,广州510075; 2. 吉林大学地球科学学院,长春130061
基金项目:国家专项,国家重点基础研究发展计划"973"项目 
摘    要:华南陆缘中生界地层以广东省出露最广,这套地层为陆源碎屑沉积岩,局部为火山岩。上三叠统—上白垩统划分为2个巨层序、7个超层序和15个层序。沉积充填序列展示出本地区经历了海侵-海退过程,沉积环境由海相转化为陆相环境。3个级别的海平面变化控制了层序、超层序和巨层序的发育。粤中--粤东地区中生界发育的Ⅲ级层序可归纳出3种类型:浅水型、深水型和湖盆型;浅水型层序又可以分为浅水Ⅰ型和浅水Ⅱ型。

关 键 词:南海  华南陆缘  中生代  层序地层  海平面变化

Mesozoic sequence stratigraphic model and sea level change of South China continental margin of South China Sea
WANG Liao-liang,XU Zhong-jie,ZHANG Li,LI Fei,CHENG Ri-hui.Mesozoic sequence stratigraphic model and sea level change of South China continental margin of South China Sea[J].World Geology,2010,29(3):431-441.
Authors:WANG Liao-liang  XU Zhong-jie  ZHANG Li  LI Fei  CHENG Ri-hui
Institution:1.Guangzhou Bureau of Marine Geology Survey,Guangzhou 510075,China;2.College of Earth Sciences,Jilin University,Changchun 130061,China
Abstract:The Mesozoic strata of the continental margin in South China are widely exposed in Guangdong,including continental clastic sedimentary rocks mainly,and volcanic rocks partly.The Upper Triassic-Upper Cretaceous can be divided into 2 mega-sequences,7 supper-sequences and 15 sequences,showing a process of transgression-regression during the sedimentary environment changed from marine to terrestrial.The sea level change of the three grades controlled the development of sequences,supper-sequences and mega-sequences.The Mesozoic Ⅲ-sequence developed in central and eastern Guangdong can be concluded for 3 types,including shallow water,deep water and lacustrine basin types,and the shallow water type can be divided into types Ⅰand Ⅱ,further.
Keywords:South China Sea  South China continental margin  Mesozoic  sequence stratigraphy  sea level change
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