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The Xianshuihe fault system is a major act … The Xianshuihe fault system is a major active sinistral (left-lateral) strike-slip fault zone in southwestern China, at the eastern edge of the Tibetan Plateau. It has been responsible for many major earthquakes, and is one of the most seismically active fault zones in this part of China. active fault zones in this part of China.
, 鲜水河断裂带是中国一条大型的左旋走滑断裂带以及地震带,位于青藏高原东缘、四川省境内, … 鲜水河断裂带是中国一条大型的左旋走滑断裂带以及地震带,位于青藏高原东缘、四川省境内,以鲜水河而得名。该断裂带长约400公里、宽约200至300米,沿鲜水河谷发育。其走向为北西至南东,北起四川甘孜,向南东经炉霍、道孚、乾宁,康定,南与安宁河断裂带、小江断裂带相连。 鲜水河断裂带自中新世以来经历了多期活动,中新世中期开始从右旋走滑转为左旋走滑,左旋走滑位移量达80至100公里。目前,左旋走滑速率为8至10毫米/年。 该断裂为地震多发带,又称康定-甘孜地震带,是四川省主要的地震活动带,18世纪以来便发生过十余次6.5级以上的强震。此处最近的一次6级以上强震是2014年康定地震(6.3级)。历史上在该断裂带发生过的6.5级以上强震包括:强震是2014年康定地震(6.3级)。历史上在该断裂带发生过的6.5级以上强震包括:
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rdfs:comment |
The Xianshuihe fault system is a major act … The Xianshuihe fault system is a major active sinistral (left-lateral) strike-slip fault zone in southwestern China, at the eastern edge of the Tibetan Plateau. It has been responsible for many major earthquakes, and is one of the most seismically active fault zones in this part of China. active fault zones in this part of China.
, 鲜水河断裂带是中国一条大型的左旋走滑断裂带以及地震带,位于青藏高原东缘、四川省境内, … 鲜水河断裂带是中国一条大型的左旋走滑断裂带以及地震带,位于青藏高原东缘、四川省境内,以鲜水河而得名。该断裂带长约400公里、宽约200至300米,沿鲜水河谷发育。其走向为北西至南东,北起四川甘孜,向南东经炉霍、道孚、乾宁,康定,南与安宁河断裂带、小江断裂带相连。 鲜水河断裂带自中新世以来经历了多期活动,中新世中期开始从右旋走滑转为左旋走滑,左旋走滑位移量达80至100公里。目前,左旋走滑速率为8至10毫米/年。 该断裂为地震多发带,又称康定-甘孜地震带,是四川省主要的地震活动带,18世纪以来便发生过十余次6.5级以上的强震。此处最近的一次6级以上强震是2014年康定地震(6.3级)。历史上在该断裂带发生过的6.5级以上强震包括:强震是2014年康定地震(6.3级)。历史上在该断裂带发生过的6.5级以上强震包括:
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rdfs:label |
Xianshuihe fault system
, 鲜水河断裂带
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