曲江断裂南东段全新世滑动速率
wf(2016)
Abstract
高精度SPOT卫星影像和野外地质调查表明,曲江断裂南东段断错山前冲沟及河流Ⅰ级和Ⅱ级阶地,在探槽中见到断裂断错全新世地层,是一条右旋走滑的全新世活动断裂,兼有逆冲性质,断裂的最新活动是1970年通海7.8级地震。对曲江断裂典型走滑断错地貌进行研究,曲江断裂南东段在五街一带水平滑动速率为(3.36±0.1) mm/a,白林山一带水平滑动速率为(3.21±0.3) mm/a。
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Key words
Qujiang fault,Holocene fault,slip rate,offset landform
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