首页> 外文期刊>Izvestiya. Physics of the solid earth >Structural and seismic indications of the elements of recent and present-day stress fields in several epicentral regions of western Tien Shan
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Structural and seismic indications of the elements of recent and present-day stress fields in several epicentral regions of western Tien Shan

机译:天山西部几个震中区域近期和当前应力场要素的结构和地震指示

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摘要

This study presents the results of stress field reconstruction for the epicentral zones of large-magnitude earthquakes in some folded-mountain regions of western Tien Shan. Field studies, including geostructural and tectonophysical interpretations, performed for the Talas-Suusamyr, Chatkal-Kurama, Turkestan-Zarafshan, Gissar and Nurata-Kyzylkum regions allow the reconstruction of some regional components of the tectonic stress field. The nearly E-W orientations of the lower-order compressional axes are identified in the Chatkal-Kurama and Turkestan-Zarafshan mountain areas. Detailed structural-dynamical diagrams of several epicentral zones and reconstructions of focal mechanisms of some strong earthquakes are derived from the geostructural data. The coincidence of the present-day stress field manifested in the earthquake sources and the recent stress field derived from the geostructural determinations is revealed. The focal mechanisms of the strong earthquakes in the folded-mountain regions of western Tien Shan relate to the thrust/strike-slip faulting and breakup of large tectonic blocks.
机译:这项研究提出了在天山西部一些折叠山地区大震级地震震中区重建应力场的结果。对塔拉斯-苏萨米尔,查塔尔-库拉玛,土耳其斯坦-萨拉夫山,吉萨尔和努拉塔-基孜尔库姆地区进行的野外研究,包括地球结构和构造物理解释,可以重建构造应力场的某些区域成分。在Chatkal-Kurama和Turkestan-Zarafshan山区确定了低阶压缩轴的近似E-W方向。从地质结构数据中得出了几个震中区的详细结构动力学图和一些强地震的震源机制的重建。揭示了地震源中现今应力场与地质构造确定的最新应力场之间的一致性。天山西部折叠山地区强震的震源机制与大构造块体的冲断/走滑断层和破裂有关。

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