滇西点苍山变质杂岩中叠加低温糜棱岩的变形-变质、流体及地质意义
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  • 英文篇名:Metamorphic,deformation,fluids and geological significance of low-temperature retrogression of Diancangshan metamorphic massif along Ailaoshan-Red River strike-slip fault zone,Yunnan,China
  • 作者:程雪梅 ; 曹淑云 ; 李俊瑜 ; 喻遵谱 ; 董彦龙 ; 吕美霞 ; 刘俊来
  • 英文作者:Cheng X;Cao S;Li J;Yu Z;Dong Y;Lv M;Liu J;
  • 关键词:低温糜棱岩 ; 韧-脆性转换 ; 显微构造 ; 流体 ; 剥露 ; 流变弱化
  • 中文刊名:JDXK
  • 英文刊名:Scientia Sinica(Terrae)
  • 机构:中国地质大学地质过程与矿产资源国家重点实验室地球科学学院;中国地质大学地质过程与矿产资源国家重点实验室地球科学与资源学院;
  • 出版日期:2018-08-20
  • 出版单位:中国科学:地球科学
  • 年:2018
  • 期:v.48
  • 基金:国家重点研发计划项目(编号:2017YFC0602401);; 国家自然科学基金项目(批准号:41472188,41722207)资助
  • 语种:中文;
  • 页:JDXK201808004
  • 页数:19
  • CN:08
  • ISSN:11-5842/P
  • 分类号:35-53
摘要
点苍山变质杂岩是发育在哀牢山-红河走滑断层带上的四个变质杂岩体之一,其遭受了多阶段的变质-变形改造,特别是自晚渐新世以来其深变质岩石广泛遭受了高温韧性剪切变形及从地壳深部剥露到地表过程.本文在前人研究成果及详细的野外地质观测的基础上,对新生代点苍山杂岩的深变质岩石变形-变质作用和剥露过程开展了相关研究,尤其是重点针对叠加低温糜棱岩开展了详细的研究.其中通过光学显微镜、扫描电子显微镜的附件电子背散射衍射以及结合阴极发光技术方法和手段,开展了叠加低温糜棱岩的显微构造、变形矿物晶格优选定向以及矿物相的深入分析.研究结果表明:(1)点苍山深变质杂岩经历了早期的高温左行剪切变形以及晚期的伸展快速剥露过程,其低温变形-变质构造特征和矿物组合叠加在早期的高温变形-变质基础之上,且高温显微构造和组构部分或全部遭受晚期叠加低温剪切变形作用改造;(2)叠加低温变形-变质出现在韧-脆性转换过程中;(3)同构造剪切叠加低温变形-变质过程中的流体非常活跃,以及伴随由动态重结晶作用和/或伴随的破裂-微破裂作用导致岩石中主要组成矿物强烈细粒化,并进一步致使变形应变局部化(如微剪切带发育),其常常伴随着岩石强度的降低,并在进一步的演变过程中影响着岩石的整体流变性.
        
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