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

川西坳陷中段上三叠统须家河组二段层序地层初析
引用本文:董立全,王信.川西坳陷中段上三叠统须家河组二段层序地层初析[J].沉积与特提斯地质,2004,24(4):66-75.
作者姓名:董立全  王信
作者单位:1. 成都理工大学,四川,成都,610059
2. 成都理工大学,四川,成都,610059;中国石化西南分公司,勘探开发研究院,四川,成都,610081
摘    要:须家河组二段是川西坳陷中的区域气层。长期以来,地质分层采用岩石地层单位界面。这一界面的穿时性,造成了构造演化分析中的误差。笔者以钻井、测井和地震资料为主要研究对象,在引入地震反射“等时”约束条件的前提下,通过对须家河组长期基准面旋回层序及须二段中期基准面旋回层序的划分和对比,在建立高分辨率时间一地层格架的基础上,经过地震微相特征的仔细分析,确认须二段顶面属Ⅲ级整合界面。

关 键 词:川西坳陷  上三叠统  须家河组  层序地层
文章编号:1009-3850(2004)04-0066-10
收稿时间:2004/6/4 0:00:00

Sequence stratigraphy of the second member of the Upper Triassic Xujiahe Formation in the middle part of western Sichuan depression
DONG Li-quan,WANG Xin.Sequence stratigraphy of the second member of the Upper Triassic Xujiahe Formation in the middle part of western Sichuan depression[J].Sedimentary Geology and Tethyan Geology,2004,24(4):66-75.
Authors:DONG Li-quan  WANG Xin
Institution:DONG Li-quan~1,WANG Xin~
Abstract:The second member of the Upper Triassic Xujiahe Formation is the regional gas horizons in the middle part of western Sichuan depression. The stratigraphic horizons have long been divided according to a lithostratigraphic boundary. The diachronism of this boundary may give rise to the differences in the examination of tectonic evolution. The findings based on sequence stratigraphy in this study have disclosed that the second member of the Upper Triassic Xujiahe Formation should be the delta deposits consisting of a complete medium-term cyclic succession, including the delta plain-delta front symmetrical cyclic sequence and deepening-upward delta plain asymmetrical cyclic sequence. The top boundary of the second member of the Upper Triassic (Xujiahe) Formation is interpreted as a third-order conformity.
Keywords:western Sichuan depression  Upper Triassic  Xujiahe Formation  sequence stratigraphy
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《沉积与特提斯地质》浏览原始摘要信息
点击此处可从《沉积与特提斯地质》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