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康古尔塔格韧性剪切带变质作用研究
引用本文:徐湘康,李新峰.康古尔塔格韧性剪切带变质作用研究[J].新疆地质,1994(3).
作者姓名:徐湘康  李新峰
作者单位:新疆维吾尔自治区地质矿产局第一地质大队
摘    要:康古尔韧性剪切带是一个复杂而强烈的构造变形带,其特征表现为4个变形期次。由于韧性剪切──区域动力作用,使变质程度明显高于剪切带两侧的区域埋深变质,变质特征表现在葡萄石-绿纤石相经韧性变形作用后,形成一套低绿片岩相变质地层,体现出前进变质作用的特点──矿物普遍细粒化,并发生动态重结晶,这套低绿片岩相变质地层,为金的富集成矿提供了可靠的矿源层。

关 键 词:康古尔塔格,韧性剪切,变质作用,变形组构,前进变质,变晶结构,变余构造

METANORPHISM OF KANGURTAG DUCTILE SHEAR ZONE
Xu Xiangkang,Li Xinfeng.METANORPHISM OF KANGURTAG DUCTILE SHEAR ZONE[J].Xinjiang Geology,1994(3).
Authors:Xu Xiangkang  Li Xinfeng
Abstract:The ductile shear zone in Kangurtag went through 4-phase complicated and intensive structural deformation.Ductile shearing-regional dynamic metamorphism of the shear zone is obviously higher than regional burial metamorphism of the two sides.The metamorphism is characterized by a sequence of low greenschist phase formed by ductile shearing of ciltonite-chlorastrolite phase.It is shown as progress metamorphism,that is,the minerals mostly get fine-grained and accept dynamic recrystallization.The low-greenschist phase metamorphism supplies a reliable ore source bed for the concentration of gold.
Keywords:Kangurtag  ductile shear  metamorphism  deform fabric  progress metamorphism  meta-crystalline texture  blastostructure
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