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ISSN 2096-7780 CN 10-1665/P

熊峰, 杨彦明, 庞博, 张小艳, 王旭东, 杨红樱. 基于重力观测的巴颜喀拉块体强震震级模拟分析[J]. 地震科学进展 , 2021, (11): 481-488. DOI: 10.3969/j.issn.2096-7780.2021.11.001
引用本文: 熊峰, 杨彦明, 庞博, 张小艳, 王旭东, 杨红樱. 基于重力观测的巴颜喀拉块体强震震级模拟分析[J]. 地震科学进展 , 2021, (11): 481-488. DOI: 10.3969/j.issn.2096-7780.2021.11.001
Xiong Feng, Yang Yanming, Pang Bo, Zhang Xiaoyan, Wang Xudong, Yang Hongying. Simulation analysis of strong earthquake magnitude in Bayankala block based on gravity observation[J]. Progress in Earthquake Sciences, 2021, (11): 481-488. DOI: 10.3969/j.issn.2096-7780.2021.11.001
Citation: Xiong Feng, Yang Yanming, Pang Bo, Zhang Xiaoyan, Wang Xudong, Yang Hongying. Simulation analysis of strong earthquake magnitude in Bayankala block based on gravity observation[J]. Progress in Earthquake Sciences, 2021, (11): 481-488. DOI: 10.3969/j.issn.2096-7780.2021.11.001

基于重力观测的巴颜喀拉块体强震震级模拟分析

Simulation analysis of strong earthquake magnitude in Bayankala block based on gravity observation

  • 摘要: 以内蒙古乌加河地震台的连续重力观测资料为基础,应用PET重力仪采样率较高的特点,分析了PET相对重力仪与JCZ-1甚宽带地震仪的波形相关关系及同震形变物理特征。通过模拟分析乌加河地震台PET相对重力仪记录到巴颜喀拉块体周围发生的6次7级以上强地震的同震P波、S波及面波与震中距离、震级的相关关系,得出一般震级模型、地应力波模型和S波P波幅度比模型公式。通过计算3种震级模型理论震级与实际震级的误差及相关系数R值,得到理论震级与实测震级标准误差达到0.04,R值达到0.99,验证了模型的可靠性。对比分析理论震级与实际震级的误差与R值,揭示同震形变波形蕴含地球动力特征的物理机制。

     

    Abstract: Based on the continuous gravity observation data of Wujiahe seismic station in Inner Mongolia, the waveform correlation between PET relative gravimeter and JCZ-1 very broadband seismometer and the physical characteristics of coseismic deformation are analyzed using the high sampling rate of PET gravimeter. By simulating and analyzing the correlation between the coseismic P-wave, S-wave and surface wave with epicentral distance and magnitude of six strong earthquakes with M≥7 occurred around Bayankala block recorded by PET relative gravimeter at Wujiahe seismic station, the general magnitude model, in-situ stress wave model and S-wave P-wave amplitude ratio model are obtained. By calculating the error and correlation coefficient R value between the theoretical magnitude and the actual magnitude of the three models, the standard error between the theoretical magnitude and the measured magnitude is 0.04, and the R value is 0.99, which verifies the reliability of the model. The error and R value of theoretical magnitude and actual magnitude are compared and analyzed to reveal the physical mechanism of geodynamic characteristics contained in coseismic deformation waveform.

     

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