Elsevier BV
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Structural characteristics of the basement and the prospective of favorable oil and gas blocks in the Tacheng basin
Elsevier BV - Tập 25 Số 5-6 - Trang 527-534 - 2012
Ground motion prediction equations based on shallow crustal earthquakes in Georgia and the surrounding Caucasus
Elsevier BV - Tập 35 - Trang 497-509 - 2022
S-wave velocity structure in the SE Tibetan plateau
Elsevier BV - Tập 29 - Trang 165-172 - 2016
We use observations recorded by 23 permanent and 99 temporary stations in the SE Tibetan plateau to obtain the S-wave velocity structure along two profiles by applying joint inversion with receiver functions and surface waves. The two profiles cross West Yunnan block (WYB), the Central Yunnan sub-block (CYB), South China block (SCB), and Nanpanjiang basin (NPB). The profile at ~25°N shows that the......
The gravity and isostatic Moho in North China Craton and their implications to seismicity
Elsevier BV - Tập 27 Số 2 - Trang 197-207 - 2014
Heterogeneous strain regime in the eastern margin of Tibetan Plateau and its tectonic implications
Elsevier BV - Tập 28 - Trang 1-10 - 2015
The eastern margin of Tibetan Plateau is one of the most active zones of tectonic deformation and seismicity in China. To monitor strain buildup and benefit seismic risk assessment, we constructed 14 survey-mode global position system (GPS) stations throughout the northwest of Longmenshan fault. A new GPS field over 1999–2011 is derived from measurements of the newly built and pre-existing station......
1-D P- and S-wave velocity models for the collision zone between the northern Tianshan mountain and the Junggar basin based on local earthquake data
Elsevier BV - Tập 25 - Trang 495-503 - 2012
We have developed crustal minimum 1-D P- and S-wave velocity models of the collision zone between the northern Tianshan mountain and the Junggar basin (86°E–89°E, 43°N–44.5°N). These two models were created through inversion of 1 370 P- and 1 396 S-wave travel times from 173 well-constrained local earthquakes recorded by the Ürümqi sparse local seismic network and temporary seismic arrays. In cont......
Depth determination of the Moho interface beneath the Tibetan plateau and other areas of China
Elsevier BV - Tập 25 - Trang 415-431 - 2012
We apply the adaptive moving window method of Sun et al. to the most recent catalog data and the data recorded by portable stations to construct the velocity structure of the crust and upper mantle, and to determine the depth of the Moho interface beneath the Tibetan plateau and other areas of China. We first select 2 600 locations in the study region with 1° intervals, then at each location inver......
Near-field triggering of microearthquakes along the Longitudinal Valley fault in eastern Taiwan*
Elsevier BV - Tập 33 - Trang 273-280 - 2020
A note on the equivalence of three major propagator algorithms for computational stability and efficiency
Elsevier BV - Tập 25 - Trang 55-64 - 2012
It is shown in this note that the three methods, the orthonormalization method, the minor matrix method and the recursive reflection-transmission matrix method are closely related and solve the numerical instability in the original Thomson-Haskell propagator matrix method equally well. Another stable and efficient method based on the orthonormalization and the Langer block-diagonal decomposition i......
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