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神奇美丽的横断山:地壳演化塑造的奇迹——“三江并流”世界自然遗产地形成地质背景浅析
引用本文:王义昭.神奇美丽的横断山:地壳演化塑造的奇迹——“三江并流”世界自然遗产地形成地质背景浅析[J].地质通报,2006(Z1).
作者姓名:王义昭
作者单位:云南省区域地质调查队 云南玉溪653100
摘    要:三江并流是反映地球演化主要阶段的杰出代表,区内保存着反映特提斯演化不同阶段和喜马拉雅期陆内造山阶段留下的丰富的地质遗迹,这些地质遗迹为解读三江并流地壳演化的历史提供了重要的依据。有关资料表明,三江并流是与青藏高原和横断山脉一起发育成长起来的,它们均经历了特提斯的演化,并且都是印度板块与欧亚板块强烈碰撞造山作用的产物。本文比较详细地介绍了横断山脉的形成演化过程及其与青藏高原形成演化之间的关系。

关 键 词:横断山  三江地区  三江并流自然遗产地  青藏高原  特提斯  喜马拉雅碰撞造山作用

Mystical and beautiful Hengduan Mountains: a miracle made by crustal evolution-Analysis of the geological background for "confluence of three rivers".
WANG Yi-zhaoRegional Geological Survey Party of Yunnan Province,Yuxi ,Yunnan,China.Mystical and beautiful Hengduan Mountains: a miracle made by crustal evolution-Analysis of the geological background for "confluence of three rivers".[J].Geologcal Bulletin OF China,2006(Z1).
Authors:WANG Yi-zhaoRegional Geological Survey Party of Yunnan Province  Yuxi  Yunnan  China
Institution:WANG Yi-zhaoRegional Geological Survey Party of Yunnan Province,Yuxi 653100,Yunnan,China
Abstract:The "confluence of three rivers" is an outstanding representative reflecting the main stage of evolution of the Earth. Abundant geological remains reflecting different stages of Tethys evolution and Himalayan intracontinental orogenic stage are preserved in the study area. These geological remains provide an important basis for the interpretation of the history of crustal evolution marked by confluence of three rivers. Relevant data indicate that confluence of three rivers occurred together with the formation of the Qinghai-Tibet Plateau and the Hengduan Mountains. They all experienced the evolution of the Tethys and are all the product of strong collisional orogeny of the Indian plate and Eurasian plate. This paper introduces in details the formation and evolution of the Hengduan Mountains and their relation to the formation and evolution of the Qinghai-Tibet Plateau.
Keywords:Hengduan Mountains  Sanjiang region  site of natural heritage of confluence of three rivers  Qinghai-Tibet Plateau  Tethys  Himalayan collisional orogeny
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