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郯庐断裂南段主断裂韧性剪切带形成历时时限的探索
引用本文:刘德良,曹高社,李振生,杨晓勇,巩翔.郯庐断裂南段主断裂韧性剪切带形成历时时限的探索[J].地学前缘,2002,9(2):475-482.
作者姓名:刘德良  曹高社  李振生  杨晓勇  巩翔
作者单位:中国科技大学,地球与空间科学学院,第三世界科学院,地球科学和天文学高级研究中心,安徽,合肥,230026
基金项目:国家自然科学基金资助项目 ( 4 0 172 0 72 ),国家“九五” 重点科技攻关资助项目 ( 96 110 )
摘    要:为求得此前未曾测得过的郯庐断裂韧性构造事件的过程时间 ,选定居于安徽省肥东县桴槎山隶属郯庐断裂南段主断裂韧性剪切带糜棱岩为研究对象。运用显微构造物理化学方法 ,首先测算形成糜棱岩的差异流动应力 ,以进行应变速率 ( ε)的求算 ;然后 ,用等浓度线法和晶胞参数法分别测算糜棱岩化过程中岩石体积应变量 (fV) ;再根据公式t =-lnfV/ ε ,计算出糜棱岩化过程时间 (t)。结果得出该糜棱岩带的形成时限为几十万年 (0 19~ 0 94Ma)的时间跨度 ,不同方法测定时限的精度差值在半个量级左右。

关 键 词:构造形成时限  晶胞参数法  等浓度线法  应变速率  流动应力  韧性剪切带  郯庐断裂
文章编号:1005-2321(2002)02-0475-08
修稿时间:2002年1月1日

DURATION TIME OF STRUCTURAL DEFORMATION FOR THE DUCTILE SHEAR ZONE IN THE SOUTH OF TANCHENG-LUJIANG FAULT
LIU De\|liang,CAO Gao\|she,LI Zhen\|sheng,YANG Xiao\|yong,GONG Xiang.DURATION TIME OF STRUCTURAL DEFORMATION FOR THE DUCTILE SHEAR ZONE IN THE SOUTH OF TANCHENG-LUJIANG FAULT[J].Earth Science Frontiers,2002,9(2):475-482.
Authors:LIU De\|liang  CAO Gao\|she  LI Zhen\|sheng  YANG Xiao\|yong  GONG Xiang
Abstract:To calculate the duration time of Tancheng\|Lujiang Fault's ductile tectonic event that has never been measured, the research object we selected is the mylonite of the ductile shear zone of main fault in the south of Tancheng\|Lujiang Fault, Fucha Hill,Feidong County,Anhui Province.First,by using the physicochemical methods for microstructure,the different flow stress causing the formation of the mylonite was measured,and the strain rates were calculated.Then,by using isoconcentration line and cell parameter, the volume strain capacity was calculated.Finally, by using the expression t =-ln f V/ ,the duration time of structural deformation for the ductile shear zone was calculated.The result shows that the duration time is about hundreds of thousands years(0 19~0 94Ma) with a half magnitude of precision inaccuracy among different measures.
Keywords:duration time of structural deformation  cell parameter  isoconcentration line  strain rates  flow stress  ductile shearing zone  Tancheng\|Lujiang Fault
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