首页|2021年四川泸县MS6.0地震震源参数研究

2021年四川泸县MS6.0地震震源参数研究

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2021年9月16日四川泸县发生了有记载以来震级最大的地震(MS6.0).为了认识该地震的发震机理,我们综合使用近震和远震波形数据精确测定了 2021年泸县地震及MS≥3.0余震的机制解、深度、水平位置、破裂方向等震源参数.震源机制解结果显示这些地震大多是逆冲型,伴有少量走滑成分,MS6.0地震质心深度为4 km,矩震级为MW5.25,两个节面的走向角、倾角、滑移角分别为95°/47°/84°和283°/43°/96°;sPL和sP两个震相的波形拟合结果表明其质心深度在5 km左右.我们还利用InSAR形变资料获取了 MS6.0地震的质心位置,然后利用面波到时差相对定位方法确定了其他地震的水平位置.基于经验格林函数法得到MS6.0地震破裂方向大致为北西西.2021年泸县MS≥3.0地震质心深度在3~5 km,且质心震中位于页岩气开采注水井3 km以内,具体的发震机理还需要参考工业生产数据,通过岩石物理实验和地质力学模拟来进一步研究.
Research on the source parameters of the 2021 Luxian MS6.0 earthquake
On September 16,2021,a MS6.0 earthquake occurred in the Luxian County,Sichuan Province,which is the largest earthquake ever recorded in this area.To understand seismogenic mechanism of this earthquake,we use regional and teleseismic waveform data to precisely obtain the source parameters of the 2021 Luxian earthquake and its MS≥3.0 aftershocks,e.g.focal mechanism,depth,centroid location,and rupture directivity.Focal mechanism solutions show that most of the earthquakes in the study area have thrusting focal mechanisms,accompanied by a small strike-slip component.The centroid depth of the MS6.0 earthquake is 4 km with a moment magnitude(MW)of 5.25.The strike,dip,rake of the two nodal planes are 95°/47°/84° and 283°/43°/96°,respectively.Waveform modeling of the sPL and sP phases suggests a centroid depth of around 5 km.We also use InSAR deformation data to determine the precise centroid of the MS6.0 earthquake,and thereafter use differential travel times of surface waves to relocate the MS ≥3.0 aftershocks.Rupture directivity of the MS6.0 earthquake is in the direction of NWW inferred from an empirical Green's function method.The Luxian earthquake and its aftershocks have centroid depths of 3~5 km and are located within 3 km away from fluid injection wells of shale gas production.To understand their specific seismogenic mechanisms,it is also necessary to take industrial production data,petrophysical experiments and geomechanical simulation into consideration.

Luxian earthquakeFocal mechanismDepth phaseRelative relocationRupture directivity

莫丽桦、储日升、谷旺旺、盛敏汉、马海超、李雪垒

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中国科学院精密测量科学与技术创新研究院大地测量与地球动力学国家重点实验室,武汉 430077

中国科学院大学地球与行星科学学院,北京 100049

湖南工商大学微电子与物理学院,长沙 410205

四川泸县 震源机制解 深度震相 相对定位 破裂方向

国家自然科学基金中国科学院战略性先导科技专项(B类)国家自然科学基金国家自然科学基金湖北省科技创新人才专项湖南省教育厅科研项目

42325401XDB41020202U20A2095420040432022EJD01521B0566

2024

地球物理学报
中国地球物理学会 中国科学院地质与地球物理研究所

地球物理学报

CSTPCD北大核心
影响因子:3.703
ISSN:0001-5733
年,卷(期):2024.67(4)
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