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| THE GEOTECTONICS AND SIGNIFICANCE OF HAILAR-XINZHANGFANG FAULT ZONE |
| LIU Bao-shan1, LI Yang-chun1, ZHANG Yu2,3 |
1. Qiqihar Branch, Heilongjiang Institute of Regional Geological Survey, Qiqiharr 161005, China;
2. China University of Geosciences, Beijing 100083, China;
3. Heilongjiang Institute of Regional Geological Survey, Harbin 150036, China |
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Abstract The Hailar-Xinzhangfang faulted zone in Daxinganling area is a multi-stage moved fault,which provides space for the emplacement and eruption of magmatic activities during Mesozoic era,and controls the distribution of Mesozoic geologic bodies.The geologic bodies on each sides of the fault are different in distribution and scale.A regional geological survey and mapping in this area reveals that the Hailar-Xinzhangfeng faulted zone is a large strike-slip fault.It displays various structural characters in different periods.The fault is also the demarcation line of regional tectonic elements.On the east is upwelling area,whille down warping region on the west.
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Received: 04 March 2003
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| [1] |
CHEN Hui-jun, CUI Tian-ri, QIAN Cheng, LI Lin-chuan, CHEN Jing-sheng, LI Wei, WU Xin-wei, JIANG Bin, SI Qiu-liang, QIN Tao, TANG Zhen, ZHANG Yu-jin, GUO Wei. ZIRCON U-Pb GEOCHRONOLOGY OF BASHENGHE PLUTON IN NORTHERN DAXINGANLING MOUNTAINS: Geological Implications[J]. GEOLOGY AND RESOURCES, 2019, 28(5): 405-412. |
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2003, Vol. 12 
