检索结果-南通市图书馆

检索条件"主题词=Southern flank of Tianshan Mountains"

共 1 条记录，以下是1-10 订阅

全选清除本页清除全部题录导出标记到"检索档案"

详细简洁

排序：

Late Cenozoic transtensional fault belt discovered on the boundary of the Awati Sag in the northwestern Tarim Basin

Late Cenozoic transtensional fault belt discovered on the bo...

引用

中国科学院地质与地球物理研究所2015年度（第15届）学术年会

作者： Yue?Jun Li Qiang Zhang Guang?Ya Zhang Hai?Jun Yang Xian?Zhang Yang Jun Shi Yuan Neng Yan?Gui Chen Lei Wen Institute of Geology and Geophysics Chinese Academy of Sciences Research Institute of Petroleum Exploration and Development Petro China Tarim Oilield Company PetroChina

Late Cenozoic transtensional fault belt was discovered on Shajingzi fault belt,NW boundary of the Awati Sag in the northwestern Tarim *** numerous Quaternary normal faults were discovered on Aqia and Tumuxiuke fault belts,SW boundary of *** discovery reveals Quaternary normal fault activity in the Tarim Basin for the irst *** is also a new discovery in the southern flank of tianshan *** transtensional fault belt is made up of numerous,small normal ***,the normal faults are arranged in right-step,en echelon patterns along the preexisting Shajingzi basement fault,forming a sinistral transtensional normal fault *** proile,they cut through the Paleozoic to the mid-Quaternary and combine to form negative flower *** Late Cenozoic normal faults on the SW boundary of Awati Sag were distributed mainly in the uplift side of the preexisting Aqia and Tumuxiuke basement-involved faults,and combined to form small horst and graben structures in *** on the intensive seismic interpretation,careful fault mapping,and growth index analysis,we conclude that the normal fault activity of Shajingzi transtensional fault belt began from Late Pliocene and ceased in Late Pleistocene(mid-Quaternary).And the normal faulting on the SW boundary of Awati Sag began from the very beginning ofQuaternary and ceased in *** normal faulting on Awati’s SW boundary began a little later than those on the NW *** origin of Shajingzi transtensional normal fault belt was due to the left-lateral strike-slip occurred in the southern flank of tianshan,and then,due to the eastward escape of the Awati block,a tensional stress developed the normal faults on its SW boundary.

关键词： Pliocene–Pleistocene normal fault Late Cenozoic transtensional normal fault belt Left-lateral strike-slip Awati Sag Northwestern Tarim Basin southern flank of tianshan mountains Seismic interpretation

来源： cnki会议评论

在线全文

cnki会议

学校读者我要写书评

暂无评论

全选清除本页清除全部题录导出标记到“检索档案”

共1页 << < 1 > >>

回到顶部

执行限定条件

欢迎您,

建议与咨询留下您的常用邮箱和电话号码，以便我们向您反馈解决方案和替代方法

时间限定

文献类型

馆藏选择

核心期刊

语言

文献类型

帮助

文字说明：

检索规则说明：

检索范例：

分类表

所选分类

限定检索结果

文献类型

馆藏范围

日期分布

学科分类号

主题

机构

作者

语言

在线全文

请选择保存的检索档案：

请选择收藏分类：

通借通还

欢迎您,

建议与咨询 留下您的常用邮箱和电话号码，以便我们向您反馈解决方案和替代方法

时间限定

文献类型

馆藏选择

核心期刊

语言

文献类型

帮助

文字说明：

检索规则说明：

检索范例：

分类表

所选分类

限定检索结果

文献类型

馆藏范围

日期分布

学科分类号

主题

机构

作者

语言

在线全文

请选择保存的检索档案： 新增检索档案 确定 取消

请选择收藏分类： 新增自定义分类 确定 取消

通借通还

建议与咨询留下您的常用邮箱和电话号码，以便我们向您反馈解决方案和替代方法

请选择保存的检索档案：

请选择收藏分类：