杨宇^1,2,,
雷建设^2,,,
张广伟²,
梁姗姗³,
孙长青²,
米琦²,
鲁明文²,
杜沫霏²,
张冰²,
田凡凡²,
何静²,
王健²,
吴宝峰⁴,
马晨²,
刘泽民²
1. 中国地震局地球物理研究所, 北京 100081
2. 中国地震局地壳应力研究所(地壳动力学重点实验室), 北京 100085
3. 中国地震台网中心, 北京 100045
4. 黑龙江省地震局, 哈尔滨 150090

基金项目: 国家自然科学基金重点项目（41530212），面上项目（41674901，41474040），中国地震局地壳应力研究所基本科研业务专项（ZDJ2017-15），中国科学院战略性先导科技专项（B类）（XDB18000000）和国家重点研发计划项目（2016YFC 0600408）联合资助


详细信息

作者简介: 杨宇, 女, 1990年生, 博士研究生, 主要从事地震波层析成像方面的研究.E-mail:lyanla1990@163.com

通讯作者: 雷建设, 男, 1969年生, 博士, 研究员, 主要从事地震波层析成像理论与应用研究.E-mail:jshlei_cj@hotmail.com

中图分类号: P315

收稿日期:2019-01-18
修回日期:2019-06-04
上线日期:2019-11-05

Crustal velocity structure and seismogenic environment in the source areas of the Qianguo M_S5.8 and Songyuan M_S5.7 earthquakes

YANG Yu^1,2,,
LEI JianShe^2,,,
ZHANG GuangWei²,
LIANG ShanShan³,
SUN ChangQing²,
MI Qi²,
LU MingWen²,
DU MoFei²,
ZHANG Bing²,
TIAN FanFan²,
HE Jing²,
WANG Jian²,
WU BaoFeng⁴,
MA Chen²,
LIU ZeMin²
1. Institute of Geophysics, China Earthquake Administration, Beijing 100081, China
2. Key Laboratory of Crustal Dynamics, Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China
3. China Earthquake Networks Center, Beijing 100045, China
4. Heilongjiang Province Earthquake Administration, Harbin 150090, China


More Information

Corresponding author: LEI JianShe,E-mail:jshlei_cj@hotmail.com

MSC: P315

--> Received Date: 18 January 2019
Revised Date: 04 June 2019
Available Online: 05 November 2019


摘要
摘要:为了解2013年11月23日吉林前郭M_S5.8和2018年5月28日吉林松原M_S5.7地震震源区的地壳速度结构及其孕震环境，本研究收集了东北地区CEA固定台站、NECESSArray流动台站和五大连池WAVESArrary流动台站的连续波形数据，使用背景噪声成像方法，获得了前郭地震和松原地震震源区地壳S波速度结构.结果显示，这两个地震主要发生在相对高波速异常区，而震源区下方存在明显低波速异常，且该低速层呈北北东走向，并有向北延展的趋势.结果表明，震源区相对高波速异常区易于积累能量孕育地震，而震源区下方的低波速异常可能代表了流体作用.这种流体作用会降低断层面有效正应力从而触发地震.这种流体作用可能和太平洋板块深俯冲至我国东北地区（包括前郭地震和松原地震震源区）下方的地幔转换内形成"大地幔楔"结构与动力学密切相关.在"大地幔楔"结构中，由于地幔转换带中滞留板块脱水作用和地幔角流作用，容易形成热湿物质上涌，进而导致松辽盆地中北部岩石圈物质拆沉、地幔流体入侵至中下地壳、然后作用于断裂带，从而导致了两个震源区中强度地震的发生.
关键词: 背景噪声成像/
松原地震/
前郭地震/
地壳速度结构/
孕震环境

Abstract:To understand the crust velocity and seismogenic environment of the 23 November 2013 Qianguo, Jilin, M_S5.8 earthquake and 28 May 2018 Songyuan, Jilin, M_S5.7 earthquake, we collect the continuous waveform data from CEA permanent seismic stations, NECESSArray portable seismic stations, and WAVESArray portable seismic stations, apply the ambient noise tomographic technique to infer the 3-D S-wave velocity structure of the crust both in the Songyuan and Qianguo earthquake source areas. The results show that these two earthquakes occurred in the relative high-velocity areas, and the source areas are underlain by an obvious low-velocity anomaly with a NNE-SSW orientation and a northward extension. These results suggest that the source areas with relative high velocities are easier to accumulate the energy and generate the earthquakes, whereas the low-velocity anomaly under the source areas may denote the influence of fluids. These fluids influence could be related to the big mantle wedge structure and dynamics due to the deep subduction of the Pacific slab down to the mantle transition zone under NE China including the Qianguo and Songyuan earthquake source areas. In the big mantle wedge structure, owing to the dehydration reaction of the stagnant slab in the mantle transition zone and corner flow, there exists hot and wet mantle upwelling which leads to the lithospheric delamination under the central-to-north Songliao basin, and the mantle fluids can intrude to the mid-lower crust and affect the fault zone. These processes could result in the generation of these two earthquakes.
Key words:Ambient noise tomography/
Songyuan earthquake/
Qianguo earthquake/
Crustal velocity structure/
Seismogenic environment



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