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DOI:
地质力学学报:1995,1(1):53-59
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雅鲁藏布江断裂带的形成
ON THE FORMATION OF YARLUNG ZANGBO RIVER FAULT ZONE
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中文摘要: 雅江断裂带主要由4条断层组成3个向西南突出的巨大弧形断裂带。晚三叠世至第四纪,雅江断裂带都有沉积地层发育,从西北向东南,各弧形断裂带成为相继接受沉积的坳陷区,而同一时期,与之紧邻的南北两盘却为隆升区。雅江断裂带,正是在该区地壳多次层波运动中形成的。
Abstract:The Yarlung Zangbo River fault zone cosists of four arcuate faults bending towards the southwest. The fault zones had become successively subsided from the northwest to the southeast to receive sediments from late Triassic up to the Quaternary,with the adjoining regions uplifted. The crustal movement that brought about the fault zone are characterized by an uplifting on the north and subsidence on the south of the region,the latter becoming subsequently elevated.
文章编号:     中图分类号:P542.3    文献标志码:
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Lao Xiong Institute of Geology, CAGS 
引用文本:
劳雄,1995.雅鲁藏布江断裂带的形成[J].地质力学学报,1(1):53-59.DOI:
Lao Xiong,1995.ON THE FORMATION OF YARLUNG ZANGBO RIVER FAULT ZONE[J].Journal of Geomechanics,1(1):53-59.DOI:

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