Inverting Anisotropy and Crustal Velocity Structure beneath Taiwan Region from Tele-Seismic Receiver Functions

碩士 === 國立中正大學 === 應用地球物理研究所 === 99 === Taiwan is located at the convergent boundary of the Eurasia plate and the Philippine Sea Plate. Philippine Sea Plate is extruding to N-W direction, so the complex collision mechanism make big lateral variation of Geotectonics beneath Taiwan. In the past, many g...

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Bibliographic Details
Main Authors: Wang, Pengkang, 王鵬綱
Other Authors: Chen, Chauhuei
Format: Others
Language:zh-TW
Published: 2011
Online Access:http://ndltd.ncl.edu.tw/handle/87021618748560392416