Mantle Potential Temperature Estimates of Basalt from the East Taiwan Ophiolite
The East Taiwan Ophiolite (ETO) is a fragment of the eastern-most South China Sea that was accreted to the Eurasian margin during the Pliocene and is a member of the Western Pacific and Cordilleran belt ophiolite group. Ophiolites from the Western Pacific and Cordilleran belt are typically subductio...
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| Format: | Article |
| Language: | English |
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Chinese Geoscience Union
2016-01-01
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| Series: | Terrestrial, Atmospheric and Oceanic Sciences |
| Online Access: |
http://tao.cgu.org.tw/media/k2/attachments/v276p853.pdf
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