Abstract The evolution of the Taiwan orogeny is often described in terms of deformation of rocks above a shallow decollement, either in a continuously deforming wedge or a discretely deforming stack of thrust sheets. Recently acquired evidence from seismic tomography, ...
CITATION STYLE
Lin, C. H., & Roecker, S. W. (1998). Active Crustal Subduction and Exhumation in Taiwan (pp. 1–25). https://doi.org/10.1007/978-94-015-9050-1_1
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