张华, 黄树生, 陆丽娟, 黄惠宁, 张帆. 广西南丹大厂矿区震源参数研究[J]. 华北地震科学, 2014, 32(3): 24-30. DOI: 10.3969/j.issn.1003-1375.2014.03.006
引用本文: 张华, 黄树生, 陆丽娟, 黄惠宁, 张帆. 广西南丹大厂矿区震源参数研究[J]. 华北地震科学, 2014, 32(3): 24-30. DOI: 10.3969/j.issn.1003-1375.2014.03.006
ZHANG Hua, HUANG Shu-sheng, LU Li-juan, HUANG Hui-ning, ZHANG fan. Study on Source Parameters of Earthquakes in Dachang Mining Area[J]. North China Earthquake Sciences, 2014, 32(3): 24-30. DOI: 10.3969/j.issn.1003-1375.2014.03.006
Citation: ZHANG Hua, HUANG Shu-sheng, LU Li-juan, HUANG Hui-ning, ZHANG fan. Study on Source Parameters of Earthquakes in Dachang Mining Area[J]. North China Earthquake Sciences, 2014, 32(3): 24-30. DOI: 10.3969/j.issn.1003-1375.2014.03.006

广西南丹大厂矿区震源参数研究

Study on Source Parameters of Earthquakes in Dachang Mining Area

  • 摘要: 利用广西南丹县大厂矿区地震监测台网记录的地震波资料,采用Brune(1970)模型,将速度记录谱归算为震源位移谱,使用遗传算法计算拐角频率及零频极限,然后计算地震矩、应力降等小震震源参数,并系统分析各种参数之间的关系。大厂矿区38次较大地震的震源参数计算结果为:地震矩范围在2.18×1011~7.89×1012 N·m之间;震源破裂半径78~439m;地震应力降在0.01~1.79 MPa之间。表明:地震矩与震级、震源半径、拐角频率之间呈线性关系,而应力降不依赖于地震矩,分布较为离散。大厂矿区应力降值明显偏低,这可能与该区域背景应力低有关。

     

    Abstract: Using the Brune model (1970)and the digital seismic wave data of the earthquake occurred in Dachang mining area,which was recorded by Guangxi Dachang seismic network;we transferred the velocity spectrum into source displacement spectrum.The corner frequency and zero frequency were calculated by using genetic algorithm,further,the source parameters including seismic moment and stress drop were calculated and the relationships among them were analyzed systematically.This paper studies 38 bigger regional earthquakes occurred in this area,the results show that they seismic moments are 2.18×1011~7.89 ×1012 Nom and rupture radius are 78~439 m,stress drop are 0.01~1.79 MPa.The relations between seismic moment,body-wave magnitude,rupture radius and corner frequency are near log-linear.The distribution of stress drop is dispersed and show little obvious correlation with seismic moment.Dachang mining stress drop values significantly lower,this may be related to the low regional background stress.

     

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