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东疆哈尔里克造山带中红柱石的变形特征及其地质意义
引用本文:赵明,王赐银.东疆哈尔里克造山带中红柱石的变形特征及其地质意义[J].矿物学报,2001,21(3):377-380.
作者姓名:赵明  王赐银
作者单位:南京大学地球科学系
基金项目:国家自然科学基金项目 (批准号 :49372 10 2 )
摘    要:东疆哈尔里克造山带中红柱石的变形显微构造与区内A型俯冲引起的断裂区域变质作用有成因联系。红柱石的变形特征显示了其变形机制为塑性形变,处于韧性变形的条件下,表明变形前形成于一定的深度,后受推覆构造作用,发生变形并被带至地表,是区内构造演化的产物。

关 键 词:哈尔里克造山带  红柱石  显微变形构造  变形机制  构造演化
文章编号:1000-4734(2001)03-0377-04
修稿时间:2001年3月23日

DEFORMATION CHARACTERISTICS OF ANDALUSITE AND THEIR GEOLOGICAL SIGNIFICANCE FROM THE HARLIK OROGENIC BELT IN EASTERN TIANSHAN
Zhao Ming,Wang Ciyin.DEFORMATION CHARACTERISTICS OF ANDALUSITE AND THEIR GEOLOGICAL SIGNIFICANCE FROM THE HARLIK OROGENIC BELT IN EASTERN TIANSHAN[J].Acta Mineralogica Sinica,2001,21(3):377-380.
Authors:Zhao Ming  Wang Ciyin
Abstract:The microfabric deformation structure of andalusite in the Harlik orogenic belt is genetically related to the faulting-induced regional metamorphism caused by intracontinental A-type subduction. The deformation characteristics of andalusite suggest that it belongs to plastic deformation under ductile metamorphic condition. It is shown that andalusite was formed at a deeper depth before deformation, then it was brought to the earth surface which was broken and deformed during large-scale thrust tectonism. It is the product of tectonic evolution in the area.
Keywords:Harlik orogenic belt  andalusite  microfabric deformation structure  deformation mechanism  tectonic evolution
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