Ages of ophiolitic rocks along plate suture in Taiwan orogen: Fate of the South China Sea from subduction to collision
Ophiolite-bearing belts mark convergent plate suture zones and are central in reconstructing plate configuration and structures of mountain belts. The active Taiwan mountain belt, product of ongoing convergence between the Eurasian and Philippine Sea plates, has dismembered ophiolitic rocks exposed...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Springer
2020-08-01
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| Series: | Terrestrial, Atmospheric and Oceanic Sciences |
| Online Access: |
http://tao.cgu.org.tw/media/k2/attachments/v314p383.pdf
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