Upper mantle P velocity structure beneath the Baikal Rift from modeling regional seismic data
Author:
Affiliation:
1. Division of Mathematics, Commonwealth Campus Pennsylvania State University Dubois Pennsylvania USA
2. Department of Geosciences Pennsylvania State University University Park Pennsylvania USA
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2002GL016115
Reference22 articles.
1. Faulting parameters and depth estimates for earthquakes in Eastern Asia;Ammon C. J.;Eos Trans. American Geophysical Union,2001
2. The Earth Flattening Transformation in Body Wave Theory
3. Paleostress reconstructions and geodynamics of the Baikal region, Central Asia, Part 2. Cenozoic rifting
4. Evidence for a seismogenic upper mantle and lower crust in the Baikal Rift
5. Seismicity, active faults and stress field of the North Muya Region, Baikal Rift: New insights on the rheology of extended continental lithosphere
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1. Pn velocity and anisotropy at the lithospheric mantle wedge beneath the middle-eastern Gangdese Metallogenic Belt, southern Tibet, China;Journal of Asian Earth Sciences;2023-12
2. Pn uppermost mantle tomography of Central Tibet: Implication for mechanisms of N-S rifts and conjugate faults;Tectonophysics;2020-08
3. Spatio-Temporal Patterns of the Development of Strong Seismic Activations (1999–2007) in the Northern Baikal Area;Russian Geology and Geophysics;2020-01-01
4. Seismicity of the Baikal rift system from regional network observations;Journal of Asian Earth Sciences;2013-01
5. Earthquake depth distributions in central Asia, and their relations with lithosphere thickness, shortening and extension;Geophysical Journal International;2011-02-09
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