| 新疆东部康古尔塔格断裂带的基本特征及地质意义 |
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| 引用本文： | 竺国强,张伯南,李忠权.新疆东部康古尔塔格断裂带的基本特征及地质意义[J].成都理工大学学报(自然科学版),1992(3). |
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| 作者姓名： | 竺国强 张伯南 李忠权 |
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| 作者单位： | 成都地质学院博物馆
(竺国强)，成都地质学院地质学系
(张伯南)，成都地质学院地质学系(李忠权) |
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| 摘 要： | 新疆东部的康古尔塔格断裂带不是板块俯冲带,而是地体的一条边界断裂带。其演化历史可分为三个主要阶段:深断裂活动阶段、韧性剪切活动阶段和断块活动阶段,并相应控制了阿齐山-黄山复合地体的形成与发展,还直接控制了黄山-镜儿泉地区铜镍含矿镁铁超镁铁杂岩体的空间展布与形态特征。
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| 关 键 词： | 新疆东部 康古尔塔格断裂带 韧性剪切带 复合地体 含铜镍矿镁铁超镁铁杂岩体 |
FUNDAMENTAL CHARACTERISTICS AND ITS GEOLOGICAL SIGNIFICANCE OF KANGGUERTAGE FAULT ZONE IN THE EASTERN XINJIANG |
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| Zhu Guoqiang,Zhang Bonan,Li Zhongquan.FUNDAMENTAL CHARACTERISTICS AND ITS GEOLOGICAL SIGNIFICANCE OF KANGGUERTAGE FAULT ZONE IN THE EASTERN XINJIANG[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1992(3). |
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| Authors: | Zhu Guoqiang Zhang Bonan Li Zhongquan |
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| Institution: | Zhu Guoqiang;Zhang Bonan;Li Zhongquan |
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| Abstract: | The geological and geophyscal data have proved that Kangguertage fault zone is an impor-tant fault zone in the eastern Xinjiang. It is not a plate subducted zone but is only a terrane boundaryfault zone. It's evolutional history can be divided into three main phases: deep fracture action, ductileShear deformation and fault block action. It controls not only the formation and development of Aqis-han-Huangshan composite terrane, but also directly the distribution and shape feature of the Cu-Ni orebearing mafic-ultramafic complex in Huangshan-Jingerquan area. |
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| Keywords: | the eastern Xinjiang Kangguertage fault zone ductile shear zone composite terrane Cu-Ni ore bearing mafic-ultramafic complex |
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