Constraints on Shear Wave Velocity Heterogeneity and Anisotropy in D” from Finite-Frequency Differential Traveltime Residual Analysis
碩士 === 國立臺灣大學 === 地質科學研究所 === 102 === The D’’ region which lies in the lowermost ~250 km of the mantle has long been postulated as a major thermo-chemical boundary layer in the earth’s dynamic evolution, where the upwelling plumes most likely originate and the downwelling cold slabs terminate. Numer...
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| Format: | Others |
| Language: | zh-TW |
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2014
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| Online Access: | http://ndltd.ncl.edu.tw/handle/89426955967067183453 |