| 龙门山南段双石断裂的特征及地质意义 |
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| 引用本文： | 林茂炳,陈运则.龙门山南段双石断裂的特征及地质意义[J].成都理工大学学报(自然科学版),1996(2). |
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| 作者姓名： | 林茂炳 陈运则 |
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| 作者单位： | 成都理工学院地质学系 |
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| 摘 要： | 双石断裂是龙门山南段的前山断裂，但并不是真正的盆地与造山带的分界。它是一组兼具走滑性质的道冲断裂，断裂带中具有许多红色地层夹片和印支期不整合残块，充分反映了该断裂发育晚于盆地的真正边界。
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| 关 键 词： | 逆冲断层，不整合残块，龙门山 |
THE CHARACTERISTIC AND GEOLOGICAL SIGNIFICANCE OF THE SHUANGSHI FAULT AT THE SOUTHERN SECTION OF LONGMEN MOUNTAINS |
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| Lin Maobing, Chen Yunze.THE CHARACTERISTIC AND GEOLOGICAL SIGNIFICANCE OF THE SHUANGSHI FAULT AT THE SOUTHERN SECTION OF LONGMEN MOUNTAINS[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1996(2). |
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| Authors: | Lin Maobing Chen Yunze |
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| Abstract: | Within the southern part of Longmen Mountains, the Shuangshi fault is the frontal fault but not the rcaly boundary between the orogenic zone and the basin. It is a thrust fault with strike-slip faults. There are many blocks of red beds and Indo-China unconformity in the fault zone. They indicate that the formation of the fault zone is later than that of the boundary of the basin. |
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| Keywords: | thrust fault unconformable residual block Longmen Mountains |
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