亚美尼亚北部地震活动与地块构造和构造活动的一般规律

Pub Date : 2020-09-23 DOI:10.5800/gt-2020-11-3-0493
K. Ghazaryan, R. Sargsyan
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引用次数: 1

摘要

研究的重点是寻找亚美尼亚北部不同地质背景下震源发生的空间规律。应用构造地貌指标界定了研究区各块体的构造活动,这些构造活动从新构造发育期开始,是在很长一段时间内表现出来的。这些块被相应地分类。考虑研究区块体构造,对区域地震活动进行了分析。确定了震源机制,确定了主要的位移趋势。通过对块体构造活动指标和不同强度地震事件位置的对比分析,确定了地震事件的空间分布规律。确定了在某些块体结构中存在不同强度的震源;震源的主要运动类型在很大程度上取决于断层结构的类型。研究这些块体的新构造活动对于发现地震事件空间分布的一般规律具有重要意义。
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General regularities of seismic activity of Northern Armenia in connection with block structure and tectonic activity
The study is focused on searching for spatial regularities in the occurrence of earthquake hypocenters in different geological settings in Northern Armenia. Tectonic-geomorphological indices are applied to define the tectonic activity of blocks composing the study area, which was manifested within a long period of time, starting from the neotectonic development period. The blocks are classified accordingly. The regional seismic activity is analysed considering the block structure of the study area. Earthquake focal mechanisms are determined, and dominant displacement trends are identified. Based on the comparative analysis of the blocks’ tectonic activity indicators and the locations of seismic events differing in strength, regular patterns of spatial distribution of seismic events are identified. It is established that the earthquake hypocenters of different strength occur in certain block structures; and the predominant types of movements in the earthquake hypocenters are largely determined by types of fault structures. It is emphasized that investigating the blocks’ neotectonic activity is important for discovering the general patterns of spatial distribution of seismic events.
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