气候变化领域集成服务门户(CCPortal): 3-D Magnetotelluric Imaging of the Easternmost Kunlun Fault: Insights Into Strain Partitioning and the Seismotectonics of the Jiuzhaigou Ms7.0 Earthquake

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DOI	10.1029/2020JB019731
	3-D Magnetotelluric Imaging of the Easternmost Kunlun Fault: Insights Into Strain Partitioning and the Seismotectonics of the Jiuzhaigou Ms7.0 Earthquake
	Sun X.; Zhan Y.; Unsworth M.; Egbert G.; Zhang H.; Chen X.; Zhao G.; Sun J.; Zhao L.; Cui T.; Liu Z.; Han J.
发表日期	2020
ISSN	21699313
卷号	125 期号:5
英文摘要	We present a three-dimensional electrical resistivity model of the crust and upper mantle beneath the easternmost Kunlun fault (EKLf), obtained by three-dimensional inversion of magnetotelluric (MT) data. The crust of the Songpan-Ganzi block is characterized by high resistivity from the surface to a depth of around 20 km, and by low resistivity in the mid-lower crust in the depth range 20–40 km. The eastern edge of the high conductivity layer is coincident with the EKLf and the Huya fault. The electrical resistivity structure provides new insights into both (1) the generation of recent M > 6 earthquakes and (2) strain partitioning on this segment of the EKLf. Our model reveals that the Huya fault is the main branch of the EKLf in the region. Together with the EKLf, the Huya fault defines the boundary between the Songpan-Ganzi and Bikou blocks. The mid-lower crust of the Songpan-Ganzi block in this region has a low resistivity that likely represents a mechanically weak layer. The 2017 Jiuzhaigou Ms7.0 earthquake and other recent M > 6 earthquakes may have been controlled by the change in viscosity in the mid-lower crust that occurs across this boundary. The high conductivity may be acting as either (1) a channel of lower crustal flow, or (2) as a weak layer that decouples the upper and lower crust. The fact that the high conductivity layer does not extend along the north side of the Sichuan Basin questions the idea that crustal flow occurs in this area. ©2020. American Geophysical Union. All Rights Reserved.
英文关键词	2017 Jiuzhaigou earthquake; 3-D inversion; High conductivity layer; Kunlun fault; Magnetotellurics
语种	英语
来源期刊	Journal of Geophysical Research: Solid Earth
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/187866
作者单位	State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing, China; Department of Physics, University of Alberta, Edmonton, Canada; College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, United States
推荐引用方式 GB/T 7714	Sun X.,Zhan Y.,Unsworth M.,et al. 3-D Magnetotelluric Imaging of the Easternmost Kunlun Fault: Insights Into Strain Partitioning and the Seismotectonics of the Jiuzhaigou Ms7.0 Earthquake[J],2020,125(5).
APA	Sun X..,Zhan Y..,Unsworth M..,Egbert G..,Zhang H..,...&Han J..(2020).3-D Magnetotelluric Imaging of the Easternmost Kunlun Fault: Insights Into Strain Partitioning and the Seismotectonics of the Jiuzhaigou Ms7.0 Earthquake.Journal of Geophysical Research: Solid Earth,125(5).
MLA	Sun X.,et al."3-D Magnetotelluric Imaging of the Easternmost Kunlun Fault: Insights Into Strain Partitioning and the Seismotectonics of the Jiuzhaigou Ms7.0 Earthquake".Journal of Geophysical Research: Solid Earth 125.5(2020).