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...

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Detalhes bibliográficos
Principais autores: Shyu, J. Bruce H., Sieh, Kerry, Chen, Yue-Gau
Formato: Journal Article
Idioma:English
Publicado em: 2012
Assuntos:
Acesso em linha:https://hdl.handle.net/10356/95774
http://hdl.handle.net/10220/8662