SEISMOLOGY AND GEOLOGY ›› 1994, Vol. 16 ›› Issue (2): 146-146.
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Ren Jinwei
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任金卫
基金资助:
地震科学联合基金资助(92202)
摘要：
则木河断裂是青藏高原东边缘鲜水河～小江断裂带中段的一条走向北北西的活动断裂。第四纪以来具有左旋走滑为主的运动特征。
Ren Jinwei. LATE QUATERNARY DISPLACEMENT AND SLIP RATE OF ZEMUHE FAULT IN SICHUAN, CHINA[J]. SEISMOLOGY AND GEOLOGY, 1994, 16(2): 146-146.
任金卫. 则木河断裂晚第四纪位移及滑动速率[J]. 地震地质, 1994, 16(2): 146-146.
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