1903年5月15/28日东安纳托利亚(土耳其)地震——基于俄罗斯帝国期刊的信息

IF 0.3 Q4 GEOCHEMISTRY & GEOPHYSICS
R. E. Tatevossian, N. G. Mokrushina
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引用次数: 0

摘要

1903年5月15日至28日的地震并不是一个新发现的未知地震事件。对其信息背景的分析表明,此次地震未使用俄罗斯地区媒体的原始宏观地震证据。同时,对早期仪器地震记录的解释并不能提供震中的准确位置,尽管震级可以相当精确地估计出来。本研究收集了1903年5月15日/28日大震效应的原始证据,在此基础上估计了震中位置,并对震中位置的准确性进行了评价。该量级是根据先前发表的研究假设的,本文没有重新评估。最后,根据我们的研究,震中相对于以前的解决方案向北西方向移动了15 km;定位精度约8公里。总的来说,震中位置的微小变化表明了东南-西北向构造的活动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Earthquake on May 15/28, 1903, in Eastern Anatolia (Turkey) based on Information in Russian Empire Periodicals

Earthquake on May 15/28, 1903, in Eastern Anatolia (Turkey) based on Information in Russian Empire Periodicals

The earthquake on May 15/28, 1903, is not a newly discovered unknown seismic event. Analysis of its information background highlighted that original macroseismic evidences from regional Russian press contemporary to the earthquake were not used. Meanwhile interpretation of early-instrumental seismic records does not provide accurate location of the epicenter, though the magnitude can be estimated rather precisely. In this study, original evidence on macroseismic effects of May 15/28, 1903, is assembled, based on which the location of the epicenter is estimated and the accuracy thereof is evaluated. The magnitude is assumed from earlier published studies and is not re-evaluated in this paper. Finally, according to our study, the epicenter is shifted in NW direction by 15 km that relative to previous solutions; accuracy of location ca. 8 km. This, in general, small change in epicenter location shows the activity of SE–NW oriented structures.

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来源期刊
Seismic Instruments
Seismic Instruments GEOCHEMISTRY & GEOPHYSICS-
自引率
44.40%
发文量
45
期刊介绍: Seismic Instruments is a journal devoted to the description of geophysical instruments used in seismic research. In addition to covering the actual instruments for registering seismic waves, substantial room is devoted to solving instrumental-methodological problems of geophysical monitoring, applying various methods that are used to search for earthquake precursors, to studying earthquake nucleation processes and to monitoring natural and technogenous processes. The description of the construction, working elements, and technical characteristics of the instruments, as well as some results of implementation of the instruments and interpretation of the results are given. Attention is paid to seismic monitoring data and earthquake catalog quality Analysis.
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