Depth determination of the Moho interface beneath the Tibetan plateau and other areas of China

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...

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Bibliographic Details
Main Authors: Yu, Diming (Author), Su, Jinrong (Author), Sun, Youshun (Contributor), Toksoz, M. Nafi (Contributor), Morgan, Frank Dale (Contributor), Wang, Xiyu (Contributor), Liu, Jun (Contributor)
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor)
Format: Article
Language:English
Published: Seismological Society of China, 2016-10-21T18:57:37Z.
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