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首页> 外文期刊>Earthquake Research in China >The Relationship Between Strong Earthquake Activity of M_s ≥ 7.0 on the Chinese Mainland and the West Kunlun-A'nyemaqen Secondary Arcuate Tectonic Zone
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The Relationship Between Strong Earthquake Activity of M_s ≥ 7.0 on the Chinese Mainland and the West Kunlun-A'nyemaqen Secondary Arcuate Tectonic Zone

机译：中国大陆M_s≥7.0的强烈地震活动与西昆仑—阿纳玛琴次生弓形构造带的关系

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摘要

The active and quiet phenomenon of moderate strong earthquakes one year before the earthquakes with M_s ≥ 7.0, the spatial distribution characteristics of the solid tide modulating and triggering earthquakes and the strong earthquake mechanisms on the Chinese continent have been studied. The secondary arcuate tectonic zone composed of the west Kunlun-A'nyemaqen faults is believed to be a very important boundary to characterize strong earthquake activity of M_s ≥ 7.0 on the Chinese continent, that is, a boundary between the seismically active region and the quiet region of moderately strong earthquakes one year before earthquakes with M_s ≥ 7.0, and a boundary of the spatial distributions between the solid tide modulating strong earthquakes (M_s ≥ 7.0) and the non-modulating ones. It might be related with the characteristics of spatial distribution of focal mechanism solutions of strong earthquakes on the Chinese Continent.
机译：研究了M_s≥7.0地震发生前一年中度强烈地震的活跃和安静现象，固体潮调制和触发地震的空间分布特征以及中国大陆的强震机理。人们认为，由西昆仑—阿涅玛干断裂组成的次级弓形构造带是表征中国大陆M_s≥7.0强烈地震活动的非常重要的边界，即地震活跃区与安静地区之间的边界。 M_s≥7.0的地震发生前一年的中强地震的区域，以及固体潮调制强地震（M_s≥7.0）和非调制潮汐之间的空间分布边界。这可能与中国大陆强震震源机制解的空间分布特征有关。

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