globalchange  > 气候变化与战略
DOI: 10.1016/j.epsl.2021.117004
论文题名:
High-resolution seismic imaging of the plate boundary in northern Baja California and southern California using double-pair double-difference tomography
作者: Share P.-E.; Castro R.R.; Vidal-Villegas J.A.; Mendoza L.; Ben-Zion Y.
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2021
卷: 568
语种: 英语
中文关键词: double-difference tomography ; Peninsular Ranges ; Salton Trough ; seismic velocities ; tectonic and fault structure
英文关键词: Earthquakes ; Faulting ; Plates (structural components) ; Sedimentary rocks ; Structural geology ; Velocity ; Baja california ; Cerro Prieto ; Double-difference tomography ; Fault structure ; Fault zone ; Peninsular range ; Plate boundaries ; Salton Trough ; Seismic velocities ; Tectonic structure ; Tomography ; Laguna
英文摘要: We image seismic properties of the plate boundary through northern Baja California and southernmost California using a double-difference tomography and earthquake relocation algorithm that incorporates both event-pair and station-pair data. The data are derived from seismic networks in southern California (SCSN) and northern Baja California (CICESE). It comprises >700,000 travel times (P and S) associated with ∼200 seismic stations and >21,000 local earthquakes from 2003-2018, along with >2,000,000 event-pair and >1,500,000 station-pair double-differences derived from these travel times. In the upper crust, low VP values in the resultant models imply deep sediments and sedimentary rocks northwest of the Salton Sea and around the northern end of the Imperial fault. Low VS values indicate regions of rock damage at the northern ends of the Sierra Juarez fault zone and Laguna Salada fault, and the southern end of the San Jacinto fault zone (SJFZ). Shallow seismicity (d<956 km) highlights the Salton Buttes and Cerro Prieto volcanoes as high heat-flow thin crust regions. At mid to lower crustal depths, the sharpest contrast in crustal VP and most prominent low VS anomaly (V∼S3.4 km/s, VP/VS ∼ 1.9) occurs along a corridor extending northwestward from the Cerro Prieto fault (CPF), east of and subparallel to the Sierra El Mayor/Cucapah and into the southern SJFZ, indicating a continuous weak fluid-rich zone. At ∼25 km depth, we observe uppermost mantle velocities (V∼P7.8 km/s) in the eastern Salton Trough, crustal velocities (V
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/165668
Appears in Collections:气候变化与战略

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作者单位: Institute of Geophysics and Planetary Physics, University of California San Diego, La Jolla, CA, United States; Center for Scientific Research and Higher Education of Ensenada (CICESE)Baja California, Mexico; Department of Earth Sciences, University of Southern California, Los Angeles, CA, United States; Southern California Earthquake Center, University of Southern California, Los Angeles, CA, United States

Recommended Citation:
Share P.-E.,Castro R.R.,Vidal-Villegas J.A.,et al. High-resolution seismic imaging of the plate boundary in northern Baja California and southern California using double-pair double-difference tomography[J]. Earth and Planetary Science Letters,2021-01-01,568
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