李祥, 万永革, 崔华伟, 高熹微, 黄骥超, 张珊珊. 2016年1月21日青海门源MS6.4地震构造应力场[J]. 华北地震科学, 2016, 34(2): 36-41. DOI: 10.3969/j.issn.1003-1375.2016.02.007
引用本文: 李祥, 万永革, 崔华伟, 高熹微, 黄骥超, 张珊珊. 2016年1月21日青海门源MS6.4地震构造应力场[J]. 华北地震科学, 2016, 34(2): 36-41. DOI: 10.3969/j.issn.1003-1375.2016.02.007
LI Xiang, WAN Yong-ge, CUI Hua-wei, GAO Xi-wei, HUANG Ji-chao, ZHANG Shan-shan. Tectonic Stress Field of 2016, MS6.4 Menyuan, Qinghai Earthquake[J]. North China Earthquake Sciences, 2016, 34(2): 36-41. DOI: 10.3969/j.issn.1003-1375.2016.02.007
Citation: LI Xiang, WAN Yong-ge, CUI Hua-wei, GAO Xi-wei, HUANG Ji-chao, ZHANG Shan-shan. Tectonic Stress Field of 2016, MS6.4 Menyuan, Qinghai Earthquake[J]. North China Earthquake Sciences, 2016, 34(2): 36-41. DOI: 10.3969/j.issn.1003-1375.2016.02.007

2016年1月21日青海门源MS6.4地震构造应力场

Tectonic Stress Field of 2016, MS6.4 Menyuan, Qinghai Earthquake

  • 摘要: 收集2016年1月21日青海门源MS6.4地震周围震源机制解资料,应用MSATSI软件反演了震中周围应力场。结果显示:区域构造应力场最大主应力轴方位由NE向顺时针偏转至NEE向,倾伏角较小,最小主应力轴方位非均匀性特征明显,整体处于近垂直状态;最大主应力轴方位顺时针偏转,主要受青藏块体NE向运动产生的挤压作用影响,青藏块体北侧受到稳定的阿拉善块体阻挡,被迫向ES方向挤出,形成以逆冲和左旋走滑为主的构造体系;地震震源机制P和T轴与其所处应力区应力方向基本一致,表明此次地震是在区域构造应力场控制下发生的。

     

    Abstract: There occurred a MS6.4 earthquake in Menyuan county, Qinghai province, on Jan 21, 2016. The focal mechanism solutions are collected around the epicenter. Stress field of the epicenter area is inverted by using MSATSI software. The results show that the maximum principal compressive stress axis gradually changed from NE direction in west region to NEE direction in east region with small dip angle, nearly perpendicular to the active faults with azimuth of NW and NWW direction. The direction of extensional stress axis has strong inhomogeneity, but the dip angle is consistently large in study region. The rotation of the maximum principal stress was mainly caused by the Tibetan plate moving in NE direction, blocked by the hard Alashan block in the north, and forced to extrude in SE direction, which forming a left lateral strike slip and thrust regime. The P and T axes of the focal mechanism of this earthquake are more consistent with the directions of compression and tension stress axes respectively, which indicates that the earthquake occurred in the thrust and left-lateral strike slip tectonic setting of the northeastern margin of the Tibetan plateau.

     

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