globalchange  > 气候变化与战略
DOI: 10.1016/j.tecto.2021.228718
论文题名:
Seismic features of the Permian Basin Region from receiver function analysis
作者: Li P.; Huang G.-C.D.; Savvaidis A.
刊名: Tectonophysics
ISSN: 00401951
出版年: 2021
卷: 801
语种: 英语
中文关键词: Moho depth ; Permian Basin ; Receiver function ; Sedimentary velocity discontinuity ; Vp/Vs ratio
英文关键词: Seismology ; Velocity ; Waveform analysis ; Mafic intrusion ; Moment magnitudes ; Receiver function analysis ; Receiver functions ; Sedimentary basin ; Seismic waveforms ; Teleseismic events ; Two layer model ; Sedimentology ; depth ; Moho ; P-wave ; S-wave ; seismic moment ; seismic velocity ; seismic wave ; seismograph ; Permian Basin ; United States
英文摘要: We used receiver function (RF) analysis to derive new seismic models of Moho depth, crustal Vp/Vs ratio, depth of sedimentary velocity discontinuity, and corresponding sedimentary Vp/Vs ratio in the Permian Basin region from the seismic waveform data of 260 moment magnitude (Mw) ≥ 6 teleseismic events. We obtained the optimal models by searching one- and two-layer models and comparing similarity between the synthetic and observed RFs. We find the first-order velocity discontinuity in sedimentary basins is shallower than the basin basement. The Delaware Basin (DB) exhibits a bowl-shaped sedimentary velocity discontinuity, with depths ranging from 1.7 km to 5.8 km, whereas the Central Basin Platform (CBP) has a shallow sedimentary velocity discontinuity, with 0.2 km to 2.7 km depths. Moho depth ranges from 36 km to 46 km in the Permian Basin region. The median Vp/Vs ratios of the crust are 1.75, 1.79, and 1.78 in the DB, CBP, and the Diablo Platform (DP), respectively. Our interpretation of the different Vp/Vs ratio in the three subregions is that the crust in the DB includes more low-Vp/Vs-ratio felsic rocks, and the crust in the CBP and DP contains more high-Vp/Vs-ratio gabbroic and basaltic rocks from the Proterozoic and Phanerozoic mafic intrusion. © 2021
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/170840
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作者单位: Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, Austin, TX 78713, United States

Recommended Citation:
Li P.,Huang G.-C.D.,Savvaidis A.. Seismic features of the Permian Basin Region from receiver function analysis[J]. Tectonophysics,2021-01-01,801
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