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
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.
刘宝山, 李仰春, 张昱. 海拉尔-新帐房断裂带大地构造属性及其意义[J]. 地质与资源, 2003, 12(4): 201-205.
LIU Bao-shan, LI Yang-chun, ZHANG Yu. THE GEOTECTONICS AND SIGNIFICANCE OF HAILAR-XINZHANGFANG FAULT ZONE. GEOLOGY AND RESOURCES, 2003, 12(4): 201-205.
2003, Vol. 12 
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