Regional Magnitude Mwa in the Russian Far East

IF 0.3 Q4 GEOCHEMISTRY & GEOPHYSICS Seismic Instruments Pub Date : 2023-03-20 DOI:10.3103/S074792392207009X
D. A. Safonov, E. P. Semenova
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Abstract

The Yuzhno-Sakhalinsk Seismological Regional Information Processing Center (RIPC) recently used the Richter magnitude Mwa to estimate the energy level of Far Eastern earthquakes. To date, this is the most common energy characteristic in the operational catalog of the RIPC. The basis is digital waveforms of regional seismic stations emulated to the characteristics of the Wood–Anderson seismograph. In the present paper, the results of determining the magnitude Mwa in Russian Far Eastern conditions are analyzed. The magnitude determination accuracy is estimated, and station corrections are obtained. The regression relation Mwa and Japanese Meteorological Agency magnitude Mj showed a high similarity between these scales. This made it possible to use Mj as the reference when studying the features of Mwa. The regional seismic network makes it possible to correctly estimate the magnitude Mwa at a regional distance (up to about 1000 km), including for deep-focus earthquakes (up to 600 km). Transfer relations between Mwa and other mass-determined regional energy characteristics of earthquakes are obtained. The Mwa scale can be used to estimate the energy level of any earthquakes in the Kuril–Okhotsk and Sakhalin regions in the magnitude range of weak and moderately strong events and is recommended for inclusion in regional earthquake catalogs for the Russian Far East.

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俄罗斯远东地区震级为Mwa
南萨哈林斯克地震区域信息处理中心(RIPC)最近利用里氏Mwa震级估算了远东地区地震的能量水平。迄今为止,这是RIPC运行目录中最常见的能量特征。其依据是对区域地震台站的数字波形与伍德-安德森地震仪的特征进行模拟。本文分析了俄罗斯远东条件下Mwa震级的测定结果。估计了震级测定精度,得到了台站改正量。Mwa与日本气象厅震级Mj的回归关系显示出高度的相似性。这使得在研究Mwa的特征时可以使用Mj作为参考。区域地震台网使正确估计区域距离(最高约1000公里)的Mwa震级成为可能,包括深震源地震(最高600公里)。得到了Mwa与其他由质量决定的区域地震能量特征之间的传递关系。Mwa震级可用于估计千岛-鄂霍次克和库页岛地区任何地震在弱和中强震级范围内的能量水平,并建议将其列入俄罗斯远东地区的区域地震目录。
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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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