Using P-wave Triplications to Study the Mantle Transition Zone beneath the Central Iranian Plateau and Surrounding Regions
碩士 === 國立臺灣大學 === 地質科學研究所 === 103 === Iranian plateau is formed by the continental collision between Arabia and Eurasia. Recent studies of regional seismic tomography show P- and S-wave anomalies in the uppermost mantle beneath Iranian Plateau, but the structure of mantle transition zone (TZ) re...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Others |
| Language: | zh-TW |
| Published: |
2015
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| Online Access: | http://ndltd.ncl.edu.tw/handle/26753016517545697932 |