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西昆仑塔木一带山前推覆构造样式浅析

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文章导航 > 西北地质 > 2014 > 47(4): 37-46

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欧健, 李向前, 潘明宝, 贺新星, 郭刚, 许应石. 西昆仑塔木一带山前推覆构造样式浅析[J]. 西北地质, 2014, 47(4): 37-46.
引用本文: 欧健, 李向前, 潘明宝, 贺新星, 郭刚, 许应石. 西昆仑塔木一带山前推覆构造样式浅析[J]. 西北地质, 2014, 47(4): 37-46.
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OU Jian, LI Xiang-qian, PAN Ming-bao, HE Xin-xing, GUO Gang, XU Ying-shi. Structural Styles of the Piedmont Nappe of the West Kunlun Mountains[J]. Northwestern Geology, 2014, 47(4): 37-46.
Citation: OU Jian, LI Xiang-qian, PAN Ming-bao, HE Xin-xing, GUO Gang, XU Ying-shi. Structural Styles of the Piedmont Nappe of the West Kunlun Mountains[J]. Northwestern Geology, 2014, 47(4): 37-46.
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西昆仑塔木一带山前推覆构造样式浅析

  • 江苏省地质调查研究院, 江苏 南京 210018

  • 基金项目: 中国地质调查局项目"新疆西昆仑1:5万J43E009017、J43E010017、J43E010018、J43E011017、J43E011018"(1212011220631)

Structural Styles of the Piedmont Nappe of the West Kunlun Mountains

  • Geological Survey of Jiangsu Province, Nanjing 210018, China

    摘要
  • 通过大量野外地质调查以及构造剖面测制工作,根据构造样式和变形特征,将西昆仑塔木一带山前推覆构造带,由南西往北东划分为5个带,变形程度依次降低.通过对卡克巴西阿格孜构造窗的调查,显示本区域至少存在2期推覆构造活动:第一期发生在晚古生代末期,具后展式特征;第二期发生于晚新生代开始,显示出前展式特征.
    Plenty of field work and tectonic section measures have been carried out in the study area. According to tectonic and deformation characteristics, 5 tectonic zones are recognized among the nappe tectonics of western Kunlun, with the degree of distortion comes down from southwest to northeast. Researches of Kakebaxi'agezi nappe inlier show at least two-stage nappe tectonic activities in this area: end of late Palaeozoic and after late Cenozoic, which are characterized by piggyback and overstep propagation respectively.
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收稿日期:  2014-07-30
修回日期:  2014-10-25
刊出日期:  2014-12-15

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