ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
西藏察隅地区构造变形分析及特征
  
关键词:Tibet  Zayü  tectonic deformation facies  tectonic community  deformation sequence
基金项目:地质矿产部区域地质调查项目
作者单位
尹光侯 云南地勘局第三地质大队 
侯世云 云南地勘局第三地质大队 
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摘要:
Structural Features and Analysis in the Zayü Area,Tibet
      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.
YIN Guang-hou,HOU Shi-yun.1999.Structural Features and Analysis in the Zayü Area,Tibet[J].Acta Geoscientica Sinica,20(2):129-136.
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