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陕西小秦岭华阳川韧性剪切带的特征及其区域构造意义

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郭 威1,2,周鼎武3,任军锋4,周小虎1,桑海清5. 陕西小秦岭华阳川韧性剪切带的特征及其区域构造意义[J]. 地质通报, 2008, 27(6): 823-828.
引用本文: 郭 威1,2,周鼎武3,任军锋4,周小虎1,桑海清5. 陕西小秦岭华阳川韧性剪切带的特征及其区域构造意义[J]. 地质通报, 2008, 27(6): 823-828.
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GUO Wei1,2, ZHOU Ding-wu3, REN Jun-feng4, ZHOU Xiao-hu1, SANG Hai-qing5. Characteristics of the Huayangchuan ductile shear zones in the Xiaoqinling Mountains, Shaanxi, China, and its regional tectonic significance[J]. Geological Bulletin of China, 2008, 27(6): 823-828.
Citation: GUO Wei1,2, ZHOU Ding-wu3, REN Jun-feng4, ZHOU Xiao-hu1, SANG Hai-qing5. Characteristics of the Huayangchuan ductile shear zones in the Xiaoqinling Mountains, Shaanxi, China, and its regional tectonic significance[J]. Geological Bulletin of China, 2008, 27(6): 823-828.
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陕西小秦岭华阳川韧性剪切带的特征及其区域构造意义

  • 1.西北大学地质系, 陕西 西安 710069; 2. 长安大学地球科学与资源学院,陕西 西安710054;3.山东科技大学,山东 青岛 266510; 4.中国石油天然气股份有限公司长庆油田分公司,陕西 西安 710021;5. 中国科学院地质与地球物理研究所,北京 100029

Characteristics of the Huayangchuan ductile shear zones in the Xiaoqinling Mountains, Shaanxi, China, and its regional tectonic significance

  • 1. Department of Geology, Northwest University, Xi′an 710069 , Shaanxi,China;2. School of Earth Sciences and Resources Management, Chang′an University, Xi′an 710054, Shaanxi,China;3. Shandong University of Science and Technology,Qingdao 266510,Shandong,China;4. Changqing Petroleum Company, CNPC, Xi′an 710021, Shaanxi,China;5. Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China

    摘要
  • 陕西小秦岭华阳川韧性剪切带发育在新太古界太华群之中，野外调研和显微构造观察结果表明，该韧性剪切带是由构造片岩、眼球状片麻岩组成的深层次韧性剪切带，具有逆冲兼左行走滑的斜冲特征。对韧性剪切带构造片岩黑云母进行40Ar/39Ar同位素定年，获得坪年龄为419M±0.6Ma，反等时线年龄为417Ma±0.8Ma。认为华阳川韧性剪切带及其相应的小秦岭区域主导构造变形是发生于419Ma左右的秦岭加里东事件的结果。
    The Huayangchuan ductile shear zone in the Xiaoqinling Mountains, Shaanxi, formed in the Neoarchean Taihua Group complex. Field survey and microscopic observation have revealed this ductile shear zone is a deep-level zone, consisting of tectonic schist and augen gneiss, which have features of thrust and sinistral strike-slip oblique subduction. 40Ar/39Ar dating of biotite from tectonic schist in the ductile shear zone yielded a plateau age of 419±0.6 Ma and an inverse isochron age of 417±0.8 Ma. Therefore the authors think that the Huayangchuan ductile shear zone and its related regional principal tectonic deformation of the Xiaoqinling Mountains formed in the Caledonian event at 419± Ma.
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刊出日期:  2008-06-15

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