Crustal S-velocity structure and radial anisotropy beneath the southern part of central and western North China Craton and the adjacent Qilian Orogenic Belt from ambient noise tomography-Reference-Cited by-同舟云学术

Crustal S-velocity structure and radial anisotropy beneath the southern part of central and western North China Craton and the adjacent Qilian Orogenic Belt from ambient noise tomography

Published:2017-09-18 Issue:10 Volume:60 Page:1752-1768
ISSN:1674-7313
Container-title:Science China Earth Sciences
language:en
Short-container-title:Sci. China Earth Sci.

Author:

Ling Yuan,Chen Ling,Wei ZiGen,Jiang MingMing,Wang Xu

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/article/10.1007/s11430-017-9092-8/fulltext.html

Reference88 articles.

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2. Bensen G D, Ritzwoller M H, Barmin M P, Levshin A L, Lin F, Moschetti M P, Shapiro N M, Yang Y. 2007. Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements. Geophys J Int, 169: 1239–1260

3. Bensen G D, Ritzwoller M H, Yang Y J. 2009. A 3-D shear velocity model of the crust and uppermost mantle beneath the United States from ambient seismic noise. Geophys J Int, 177: 1177–1196

4. Birch F. 1961. The velocity of compressional waves in rocks to 10 kilobars: 2. J Geophys Res, 66: 2199–2224

5. Carlson R W, Pearson D G, James D E. 2005. Physical, chemical, and chronological characteristics of continental mantle. Rev Geophys, 43: RG1001

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