| 西藏措勤中-新生代沉积盆地演化 |
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| 引用本文： | 陶晓风,刘登忠,朱利东,马润则,胡新伟.西藏措勤中-新生代沉积盆地演化[J].成都理工大学学报(自然科学版),2008,35(1):103-107. |
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| 作者姓名： | 陶晓风 刘登忠 朱利东 马润则 胡新伟 |
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| 作者单位： | 成都理工大学地球科学学院,成都,610059 |
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| 基金项目： | 四川省重点学科构造地质学建设基金 |
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| 摘 要： | 措勤盆地位于西藏冈底斯地块中西段,是在古生界褶皱基底上发展起来的一个中-新生代盆地.通过对措勤盆地内发育的构造、地层、岩石及沉积相综合分析,讨论了措勤盆地与喜马拉雅构造带和班公-怒江构造带的对应演化关系,反演了措勤盆地的地质发展历史.其演化经历了盆地基底形成阶段(D-P)、复合弧后盆地演化阶段(J-E2)和高原隆升盆地消亡三个阶段(Es-现今).
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| 关 键 词： | 西藏 措勤盆地 盆地演化 冈底斯构造带 西藏措勤 新生代盆地 沉积盆地演化 Tibet basin 高原隆升 盆地演化阶段 形成阶段 盆地基底 历史 地质发展 反演 演化关系 对应 怒江 构造带 喜马拉雅 综合分析 沉积相 地层 |
| 文章编号： | 1671-9727(2008)01-0103-05 |
| 修稿时间： | 2007年3月5日 |
The evolvement of the Coqen basin of Mesozoic-Cenozoic in Tibet, China |
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| TAO Xiao-feng,LIU Deng-zhong,ZHU Li-dong,MA Run-ze,HU Xin-wei.The evolvement of the Coqen basin of Mesozoic-Cenozoic in Tibet, China[J].Journal of Chengdu University of Technology: Sci & Technol Ed,2008,35(1):103-107. |
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| Authors: | TAO Xiao-feng LIU Deng-zhong ZHU Li-dong MA Run-ze HU Xin-wei |
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| Abstract: | The Coqen basin is distributed over the westward of the Gangdise block in Tibet.It is a basin of Mesozoic-Cenozoic according to east-west.The width is 130 km.The length is 700 km.The area is about 100 000 km~2.The basement of the Coqen basin formed in the telophase of Permian and is made up of the folded strata of Paleozoic.The growth of the Coqen basin is from Jurassic to Oligocene.A comprehensive analysis of the structure,the stratum,the rock and the sedimentary facies of the Coqen basin is made in this paper,and the geologic development history of the Coqen basin is reconstructed.The evolvement of the Coqen basin has gone through three stages.The first stage is the foundation of the basin basement in Permian.The second stage is the evolvement of the complex arc back basin from Jurassic to Oligocene.The third stage is the decease of the basin since Oligocene. |
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| Keywords: | Tibet Coqen basin basin evolvement Gangdise block |
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