基于希比尼矿床第一次余震的余震面积评估

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
A. Yu. Motorin, S. V. Baranov
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引用次数: 0

摘要

摘要本文根据首次余震资料,探讨了在自然地震和采动地震条件下的余震活动区建设问题。研究区为位于希比尼地块南部的磷灰石-霞石矿床。我们研究了大量不同形状、位置和方向的余震区域。该地区的大小是根据主震和第一次余震计算出的物理和统计特征来确定的。基于误差图的判据已被用于定量地比较大量不同的变量。结果表明,选取的最优区域类型显示了1996-2022年研究区地震活动性资料定量试验的最佳结果。该技术可用于根据操作处理数据预测希比尼地块矿床自然采动地震后余震活动分布面积。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Aftershock Area Assessment Based on the First Aftershocks at the Khibiny Deposits

Aftershock Area Assessment Based on the First Aftershocks at the Khibiny Deposits

Abstract—This paper examines the construction of an aftershock activity area in conditions of natural and mining-induced seismicity based after the data on the first aftershocks. The study area is apatite–nepheline deposits located in the southern part of the Khibiny massif. A significant number of variants of aftershock regions were investigated that differ in shape, location, and orientation. The size of the area has been determined by scaling based on physical and statistical characteristics calculated from both the main shock and the first aftershocks. The criterion based on an error diagram has been used to quantitatively compare a large number of different variants. As a result, the optimal area type has been selected, which showing the best results of the quantitative test based on seismicity data on the study area for 1996–2022. The technique can be used to predict the area of aftershock activity distribution at the Khibiny massif deposits after a natural–mining-induced earthquake based on operational processing data.

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来源期刊
Izvestiya, Physics of the Solid Earth
Izvestiya, Physics of the Solid Earth 地学-地球化学与地球物理
CiteScore
1.60
自引率
30.00%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.
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