| STYLE AND CONSEQUENCE OF STRAIN PARTITION IN THE NORTHEAST MARGIN OF QINGHAI—TIBET PLATEAU |
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| 引用本文： | Shen Xuhui,Ding Guoyu,Tian Qinjian,Wei Kaibo,Chen Zhengwei[WT,”BX].STYLE AND CONSEQUENCE OF STRAIN PARTITION IN THE NORTHEAST MARGIN OF QINGHAI—TIBET PLATEAU[J].地学前缘,2000(Z1). |
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| 作者姓名： | Shen Xuhui Ding Guoyu Tian Qinjian Wei Kaibo Chen Zhengwei[WT ”BX] |
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| 作者单位： | Center for Analysis and Prediction，China Seismological Bureau，Beijing 100036，China，E\|mail:shenxh@seis.ac.cn |
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| 摘 要： | STYLE AND CONSEQUENCE OF STRAIN PARTITION IN THE NORTHEAST MARGIN OF QINGHAI—TIBET PLATEAU
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| 关 键 词： | strain partition style consequence the northeast margin of Qinghai—Tibet Plateau |
Style and Consequence of Strain Partition in the Northeast Margin of Qinghai-Tibet Plateau |
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| Shen Xuhui,et al.Style and Consequence of Strain Partition in the Northeast Margin of Qinghai-Tibet Plateau[J].Earth Science Frontiers,2000(Z1). |
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| Authors: | Shen Xuhui |
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| Abstract: | The Northeastern margin of Qinghai—Tibet plateau,here refers to the region bounded by Western Qinling fault zone and Longshoushan—Liupanshan tectonic zone, where obliquely compression deformation occurred with the NE\|trending maximum principle axis of stress, with Ordos Massif to the east, Alaxa Block to the north, and Qinghai—Tibet plateau to the southwest. The main structure in this region is Haiyuan—Gulang transpression zone. It consists of a series of active faults: the Haiyuan fault zone, the Tianjingshan fault zone, the Yantongshan fault zone and the Niushoushan—Luoshan fault zone. |
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| Keywords: | strain partition style consequence the northeast margin of Qinghai—Tibet Plateau |
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