Tandem suturing and disarticulation of the Taiwan orogen revealed by its neotectonic elements
Taiwan’s numerous active faults and folds demarcate distinct eastern and western neotectonic belts. The western belt results from the attachment and subsequent detachment of a sliver of continental lithosphere to the Eurasian continental margin. The eastern belt is the product of the s...
| Principais autores: | , , |
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| Formato: | Journal Article |
| Idioma: | English |
| Publicado em: |
2012
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| Assuntos: | |
| Acesso em linha: | https://hdl.handle.net/10356/95774 http://hdl.handle.net/10220/8662 |