| 西藏察隅地区构造变形分析及特征 |
| 点此下载全文 |
| 引用本文：尹光侯,侯世云.1999.西藏察隅地区构造变形分析及特征[J].地球学报,20(2):129-136. |
| DOI： |
| 摘要点击次数: 2685 |
| 全文下载次数: 2283 |
|
| 基金项目:地质矿产部区域地质调查项目 |
|
| 中文摘要:察隅地区属多次构造变动地带，先后经历了５次构造变形的改造与叠加，主要在三叠纪－中侏罗早期受古特提斯封闭影响而形成，中侏罗世晚期后，进一步加强与定型而成为主动大陆边缘逆冲推覆、逆冲式褶皱造山带。由４个次级构造（－建造）单元组成。可分为４种构造变形相，在各构造单元中构成了变形序列。 |
| 中文关键词:西藏察隅 构造变形相 构造群落 变形序列 |
| |
| Structural Features and Analysis in the Zayü Area,Tibet |
|
|
| Abstract:The Zayü area is a polyphase structural deformation z one.It underwent five phases of structural deformation and superimpositior.It o riginated mainly under the influence of the closing of the paleo-Tethys.After th e middle part of the Mid Jarassic,it was finalized and became an active continen tal-margin thrust-type fold orogenic belt.It is composed foursecond-order struct ure(formation)units and may be divided into four toctonic deformation facies wh ich form a deformation sequence in each tectonic unit. |
| keywords:Tibet Zayü tectonic deformation facies tectonic community deformation sequence |
| 查看全文 查看/发表评论 下载PDF阅读器 |
