刘德民.西藏定结地区变质核杂岩研究[J].地质找矿论丛,2003,(1):1-5
西藏定结地区变质核杂岩研究
THE RESEARCH ABOUT EXTENSIONAL METAMOPHIC CORE COMPLEXES IN DINGJIE, XIZANG
投稿时间:2002-06-09  修订日期:2002-09-27
DOI:10.6053/j.issn.1001-1412.2003.1. 001
中文关键词:  喜马拉雅造山带  伸展构造  变质核杂岩  定结地区  西藏自治区
英文关键词:Himalayan orogen belt  stretching structure  metamorphic core complex  Tibet  Dingjie area  Xizang
基金项目:国土资源部1:25万定结幅(H45C004003)区域地质调查项目(200013000145)资助.
作者单位
刘德民 中国地质大学, 地球科学学院, 湖北, 武汉, 430074 
摘要点击次数: 1254
全文下载次数: 1668
中文摘要:
      喜马拉雅造山带定结地区近EW向展布两条变质核杂岩带:高喜马拉雅变质核杂岩带和拉轨岗日—孜松变质核杂岩带,在研究区以拉轨岗日—孜松变质核杂岩为典型代表.该变质核杂岩带由多个变质核杂岩体组成,各变质核杂岩体具典型的三层结构.核部由两期(加里东期和喜山期)花岗岩和拉轨岗日群变质岩组成;拆离断层、韧性剪切带及糜棱岩带组成滑脱层;盖层由二叠系、三叠系浅变质岩或未变质的沉积岩系组成.
英文摘要:
      Two metamorphic core complexes zones exhibit rough East-West trending in Dingjie district in Himalayan orogen belt, i.e. the High Himalayan metamorphic core complex zone and Laguigangri-Zisong metamorphic core complex zone. The latter consists of two metamorphic core complex bodies characterized by typical three-layer framework.The nucleus is made up of twice periods of granite and Laguigangri Group's metamorphic rocks;and detachment zone, ductile shear zone and mylonite zone form the decollement zone;the caprock is constituted by sedimentary rock series of Permian and Triassic.
查看全文  查看/发表评论  下载PDF阅读器
关闭