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黔西南三叠系层序充填格架及对印支运动响应
引用本文:时国,田景春,张翔,李蓉,喻美艺. 黔西南三叠系层序充填格架及对印支运动响应[J]. 西南石油学院学报, 2010, 32(2)
作者姓名:时国  田景春  张翔  李蓉  喻美艺
作者单位:时国,张翔,李蓉(成都理工大学沉积地质研究院,四川,成都,610059);田景春(成都理工大学沉积地质研究院,四川,成都,610059;"油气藏地质及开发工程"国家重点实验室·成都理工大学,四川,成都,610059);喻美艺(贵州大学资源与环境工程学院,贵州,贵阳,550003) 
基金项目:中国石化集团公司海相前瞻性重大项目,四川省构造地质学重点学科建设项目 
摘    要:选取黔西南地区上扬子碳酸盐岩台地-右江盆地的三叠系剖面进行层序划分对比,并重点对台地边缘剖面进行研究,将三叠系划分为8个三级沉积层序.在此基础上,通过与Haq等列出的三叠纪生物地层时代进行对比,建立了黔西南地区三叠系层序充填格架.根据三级沉积层序自下而上的发育组合将三叠系划分出3个二级层序:SS1、SS2、SS3.本区层序充填特征亦反映了印支运动的3个幕次.印支Ⅰ幕,右江盆地为欠补偿型被动大陆边缘阶段,以构造沉降作用为主;印支Ⅱ幕,右江盆地进入过补偿型前陆发展阶段,由于南部板块碰撞的加强,沉积中心向西北迁移;印支Ⅲ幕,随着扬子陆块的全面隆升,西部盆地和东部台地区抬升消亡.

关 键 词:层序地层  地层充填格架  三叠系  黔西南

THE SEQUENCE FILLING FRAMEWORK OF TRIASSIC IN SOUTHWESTERN GUIZHOU AND THE RESPONSE TO INDO-CHINA MOVEMENT
SHI Guo,TIAN Jing-chun,,ZHANG Xiang,LI Rong,YU Mei-yi. THE SEQUENCE FILLING FRAMEWORK OF TRIASSIC IN SOUTHWESTERN GUIZHOU AND THE RESPONSE TO INDO-CHINA MOVEMENT[J]. Journal of Southwest Petroleum Institute, 2010, 32(2)
Authors:SHI Guo  TIAN Jing-chun    ZHANG Xiang  LI Rong  YU Mei-yi
Affiliation:SHI Guo1,TIAN Jing-chun1,2,ZHANG Xiang1,LI Rong1,YU Mei-yi3(1.Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu Sichuan,610059,China,2.State Key Laboratory of Oil , Gas Reservoir Geology , Exploitation,Chengdu Sichuan 610059,3.School of Resource , Environment Technology,Guizhou University,Guiyang Guizhou 550003,China)
Abstract:The Triassic sections across southwestern Guizhou of upper Yangtze carbonate platform-Youjiang Basin are selected to correlate the consequences,the study also focuses on the sedimentary characteristics of the platform marginal facies.According to the research above,the Triassic is divided into 8 third-order sedimentary sequences.The Triassic sequence filling framework is established by comparing the Haq biostratigraphic data.Three second-order sequences are divided,SS1,SS2,SS3,which are in accordance with g...
Keywords:sequence stratigraphy  sequence filling framework  Triassic  southwestern Guizhou
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