Abstract

The results of paleoseismological, archeological, and dendrochronological studies and published materials have yielded the date of neotectonic Utrish seismic dislocations, one of the key components in seismic hazard studies of the Western Caucasus. According to previously obtained and newly acquired data, a destructive earthquake occurred here in the 12th–13th centuries. Based on seismotectonic fault data, the lower limit of its magnitude M_W ≈ 6.9. The source is located in the Utrish Fault zone, along the coast of the Abrau Peninsula. The seismogenic role of this fault is established over the aggregate data.

中文翻译：

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Utrish地震位错的跨学科约会：西部高加索地区强烈历史地震的发生源的本地化

摘要

古地震学，考古学和树木年代学研究的结果以及已发表的材料，为新构造的Utrish地震脱位提供了日期，这是西高加索地区地震危险性研究的关键组成部分之一。根据先前获得和新获得的数据，在12至13世纪，这里发生了破坏性地震。基于地震构造的故障数据，其大小的下限中号_W¯¯ ≈6.9。震源位于阿布鲁半岛沿岸的乌特里什断层带。该断层的地震作用建立在总体数据上。