印度南部Thiruchengode Sitampundi-Kanjamalai剪切带糜棱岩的应变模式分析

T. V, Biswal T.K, Sundaralingam K, Sowmya V, Boopathi S, Mythili R
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引用次数: 1

摘要

研究了锡鲁城戈得附近北-南向Sitampundi-Kanjamalai剪切带(SKSZ)部分糜棱岩的岩石学特征和应变模式。岩石学研究表明,该区存在重结晶石英、钾长石、斜长石、黑云母和部分角闪石。利用剪切感指标对糜棱岩进行了动力学分析,如长石簇周围的再结晶型石英(石英带),S-C织物表现出右旋剪切感,SASZ部分地区表现出一定的剪切感,这可以认为是域间应变和涡度分配的产物。糜棱质叶理作用表现为北-南方向纯剪切挤压作用。进一步利用糜棱岩的L和T截面进行Flinn图法体应变分析表明,k<1处于有限应变的平坦区。采用Rxz/β法计算运动涡度值,得到0.36表示总剪切。刚性粒形图表明,纯剪切分量比单纯剪切分量更占优势。分析认为该糜棱岩经历了地壳深部700°以上的高温剪切作用。
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Strain Pattern Analysis of Mylonites From Sitampundi-Kanjamalai Shear Zone, Thiruchengode, South India
This study aims to investigate the petrography and strain pattern of mylonites from parts of N-S trending Sitampundi-Kanjamalai Shear Zone (SKSZ) around Thiruchengode. The petrographic study indicates the presence of recrystallized quartz, K-feldspar, plagioclase, biotite and some hornblende. The kinematic analysis of Mylonites was done with the help of shear sense indicators such as recrystallized type quartz (quartz ribbon) around the cluster of feldspar, S-C fabric shows dextral shear sense and some sinisterly shear sense in some parts of SASZ which can be considered as a product of partitioning of both strain and vorticity between domains. These all indicates the simple shear extension along E-W direction and the mylonitic foliation shows the pure shear compression along N-S direction. Further the study of bulk strain analysis by Flinn plot method using L and T section of mylonite shows k<1 which lies in the field of flattening zone of finite strain. The kinematic vorticity number is calculated by Rxz/β method which gives the value of 0.36 indicating the general shear. The rigid grain graph shows that the pure shear component is more ­­­­dominant than the simple shear component. The analysis leads to the conclusion that the mylonite has experienced a high temperature shearing of above 700°cat deep crustal level.
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