首页 | 本学科首页   官方微博 | 高级检索  
     检索      

二连盆地白音查干凹陷层序地层及其油气勘探意义
引用本文:李金良,樊太亮,张岳桥.二连盆地白音查干凹陷层序地层及其油气勘探意义[J].地质力学学报,2007,13(1):60-69.
作者姓名:李金良  樊太亮  张岳桥
作者单位:1.中国地质科学院地质力学研究所, 北京 100081
摘    要:基于测井和地震资料分析, 识别了二连盆地白音查干凹陷的层序界面, 建立了凹陷层序地层格架, 研究凹陷内部沉积相类型及其平面展布特征, 并建立了单断箕状断陷盆地沉积相模式。根据油气生、储、盖组合特征, 预测腾格尔组(层序Ⅲ)和都红木组一段(层序Ⅳ)为油气有利成藏层位, 南部缓坡河道砂体储集层和北部陡坡冲积扇储集层为油气有利储集相带, 达尔其断块和桑合地区为油气有利成藏区块。 

关 键 词:白音查干凹陷    层序地层    沉积相    单断箕状断陷盆地
文章编号:1006-6616(2007)01-0060-10
收稿时间:2006-07-28
修稿时间:2006年7月28日

SEQUENCE STRATIGRAPHY OF THE BAYAN QAGAN SUBBASIN IN THE EREN BASIN AND APPLICATIONS FOR PETROLEUM EXPLORATION
LI Jin-liang,FAN Tai-liang and ZHANG Yue-qiao.SEQUENCE STRATIGRAPHY OF THE BAYAN QAGAN SUBBASIN IN THE EREN BASIN AND APPLICATIONS FOR PETROLEUM EXPLORATION[J].Journal of Geomechanics,2007,13(1):60-69.
Authors:LI Jin-liang  FAN Tai-liang and ZHANG Yue-qiao
Institution:1.Institute of Geomechanics, Chinese Academay of Geological Sciences, Beijing 100081, China2.Department of Energy, China University of Geosciences, Beijing 100083, China
Abstract:Based on an analysis of well-log data and seismic profiles, the authors have identified the main sequence boundaries in the Bayan Qagan subbasin of the Eren basin, established the sequence stratigraphic framework of the subbasin and described the types of sedimentary facies and their plan distribution and constructed a sedimentary facies model of this half graben.According to the features of the source-reservoir-cap rock assemblage, the authors predict that:the Tengger Formation (sequence Ⅲ) and the first member of the Duhongmu Formation (sequence Ⅳ)are the favorable target zones for petroleum exploration, the fluvial sand bodies along the southern gentle slope and alluvial fan deposits along the northern steep slope are the favorable reservoir zones for hydrocarbon accumulation and the Da'erqi fault-block and Sanghe district are favorable blocks for hydrocarbon accumulation. 
Keywords:Bayan Qagan subbasin  sequence stratigraphy  sedimentary facies  half graben
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《地质力学学报》浏览原始摘要信息
点击此处可从《地质力学学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号