Crustal Structure beneath the Hi-CLIMB Array in Tibet from Joint Inversion of Receiver Functions and Rayleigh Wave Dispersion
碩士 === 國立臺灣大學 === 地質科學研究所 === 101 === Tibetan Plateau is a product of the continental collision between India and Eurasia beginning about 50 million years ago. The crust under Tibet has been greatly thickened and the Moho depth is the deepest of the world. In this study, we use joint inversion of re...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Others |
| Language: | zh-TW |
| Published: |
2013
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| Online Access: | http://ndltd.ncl.edu.tw/handle/73991854611427291096 |