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东秦岭陶湾岩群碳酸盐质糜棱岩的变质—变形特征及形成环境分析
引用本文:胡达,任升莲,宋传中,李加好,张妍,林寿发,李龙明,黄鹏,刘国厅.东秦岭陶湾岩群碳酸盐质糜棱岩的变质—变形特征及形成环境分析[J].地质论评,2015,61(5):1079-1088.
作者姓名:胡达  任升莲  宋传中  李加好  张妍  林寿发  李龙明  黄鹏  刘国厅
作者单位:合肥工业大学资源与环境工程学院,中国合肥,230009;;合肥工业大学资源与环境工程学院,中国合肥,230009;;合肥工业大学资源与环境工程学院,中国合肥,230009;;合肥工业大学资源与环境工程学院,中国合肥,230009;;合肥工业大学资源与环境工程学院,中国合肥,230009;;1)合肥工业大学资源与环境工程学院,中国合肥,230009;2) 滑铁卢大学,加拿大安大略省滑铁卢市,N2L 3G1;合肥工业大学资源与环境工程学院,中国合肥,230009;;合肥工业大学资源与环境工程学院,中国合肥,230009;;合肥工业大学资源与环境工程学院,中国合肥,230009;
基金项目:本文由国家自然科学基金资助项目(批准号 41272213,41072161,41272222)的成果。
摘    要:东秦岭造山带北缘的陶湾岩群中分布着一套碳酸盐质糜棱岩,具明显的塑性变形,其展布和变质变形特征严格受洛南—栾川断裂带控制,是陶湾岩群碳酸盐岩在洛南—栾川断裂带晚加里东—早海西期构造活动过程中形成的。因此,对这套碳酸盐质糜棱岩的变质—变形特征及形成环境分析,可揭示洛南—栾川断裂带在这一时期构造活动的运动学、动力学及流变学特征。本文通过野外详细的观察和测量,结合室内显微构造分析和温压条件的计算,确定其变质相属低绿片岩相,变形机制是以方解石动态重结晶和细粒化作用为主的塑性变形。变形温度为350~420℃,差异应力为50~110 MPa。石英应变椭球体形态显示陶湾岩群遭受了强烈挤压变形。所以,陶湾岩群碳酸盐质糜棱岩是在强烈的斜向挤压碰撞环境下形成的,是秦岭微陆块向华北板块下斜向俯冲碰撞的结果 。

关 键 词:陶湾岩群  碳酸盐质糜棱岩  塑性变形  断裂带  剪切作用  东秦岭
收稿时间:2014/8/18 0:00:00
修稿时间:2015/7/22 0:00:00

The Analysis on Metamorphic and Deformation Characteristics and Formation Environment of Carbonate Mylonite of Taowan Group in East Qinling
HU D,REN Shenglian,SONG Chuanzhong,LI Jiahao,ZHANG Yan,LIN Shouf,LI Longming,HUANG Peng and LIU Guoting.The Analysis on Metamorphic and Deformation Characteristics and Formation Environment of Carbonate Mylonite of Taowan Group in East Qinling[J].Geological Review,2015,61(5):1079-1088.
Authors:HU D  REN Shenglian  SONG Chuanzhong  LI Jiahao  ZHANG Yan  LIN Shouf  LI Longming  HUANG Peng and LIU Guoting
Institution:School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, 230009, China;;School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, 230009, China;;School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, 230009, China;;School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, 230009, China;;School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, 230009, China;;1) School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, 230009, China; 2)Department of Earth Sciences, University of Waterloo, Ont., N2L 3G1, Canada;School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, 230009, China;;School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, 230009, China;;School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, 230009, China;
Abstract:
Keywords:Taowan Group  carbonate mylonite  plastic deformation  fault zone  shearing action  East Qinling
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