Crustal Velocity Structure of S-Wave Beneath Tibetan Plateau with Transform Function Method-Hi-Climb Profile-Reference-Cited by-同舟云学术

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Crustal Velocity Structure of S-Wave Beneath Tibetan Plateau with Transform Function Method-Hi-Climb Profile

Published:2011-11 Issue:6 Volume:54 Page:766-776
ISSN:0898-9591
Container-title:Chinese Journal of Geophysics
language:en
Short-container-title:Chinese J. Geophys.

Author:

WANG Wei,GAO Xing¹,LI Yu-Ying,ZHANG Ya-Bin²

Affiliation:

1. State Key Laboratory of Resources and Environmental Information System, Institute of Geographic Sciences and Natural Resources Research; Chinese Academy of Sciences; Beijing; 100101; China

2. Petroleum Geophysical Prospecting Technology Research Institute of Henan Oilfield Branch Company; SINOPEC; Nanyang; 473132; China

Publisher

Wiley

Subject

General Medicine

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/cjg2.1660/fullpdf

Reference60 articles.

1. The nature of the Mohorovii discontinuity;Tseng;Chinese J. Geophys. (Acta Geophysica Sinica),1964

2. The AMSOC hole to the Earth's mantle;Hess;Trans. Am. Geophys. Union,1959

3. The origin of continents, mountain ranges and ocean basins;Kennedy;Am. Scientist.,1959

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