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南天山东段榆树沟—铜花山巨型构造混杂带的发现及意义

Discovery of Tectonic Melange Belt in the Yushugou-TonghuashanArea and Its Significance

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【作者】 陆关祥周鼎武王居里张成立

【Author】 LU Guanxiang, ZHOU Dingwu, WANG Juli, ZHANG ChengliInstitute of Environmental Science, Normal University of Beijing, Beijing, 100875Geological Department of North-west University, Xi’an, 710069

【机构】 北京师范大学环境科学系西北大学地质系西北大学地质系 100875 西北大学地质系 陕西西安 710069陕西西安 710069陕西西安 710069

【摘要】 通过遥感构造综合解析,认为南天山东段榆树沟—铜花山地区为一巨型构造混杂带。该构造带可划分为南部和北部的两带变质褶皱地层系统、中带的构造混杂系统和不同期次的岩浆侵入体。结合同位素定年和岩浆侵入的综合对比与研究,认为该地区先后经历了五期构造运动,分别为:① 南北向逆冲推覆,② 北西西向左行走滑,③ 北西西向右行走滑,④ 南北向逆冲推覆,⑤ 北北西、北东向断裂。

【Abstract】 The Yushugou-Tonghuashan area is a typical example of complex structure in orogenic belt. There are varieties of geological mass formed in different high-levels and they undergone different metamorphisms. Based on a comprehensive remote sensing structural analysis, the whole district can be subdivided into three structural belts, namely southern and northern metamorphic fold stratigraphic system, central tectonic mixed system and multi-stage intrusives. Isotopic dating of metamorphics and comparative analysis of rock types, tectonic block types and the characteristics of deformation further indicate that this area experienced five tectonic stages: (1) N-S overthrusting; (2) WNW-ESE trending sinistral strike-slipping; (3) WNW-ESE trending dextral strike-slipping; (4)N-S overthrusting; and (5) NNW and NE late-stage faulting.

【基金】 国家自然科学基金(编号 49972075);国家重点基础研究发展规划项目(编号 2001CD409801)的成果
  • 【分类号】P542.2
  • 【被引频次】7
  • 【下载频次】180
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