The Transition From An Intraoceanic Submarine Acretionary Prism To The Onland Fold-And-Thrust Belt In The Taiwan Arc-Continent Collision.

The region of Taiwan is undergoing active, oblique arc-continent colision between the Luzon Arc on the Philippine Sea Plate and the continental margin of Eurasia. The Fold-and-Thrust Belt (FTB) in Taiwan passes southwards into a submarine accretionary wedge at the Manila subduction zone. The aim of this contribution is to examine how an on land FTB changes into a marine accretionary prism in the context of an oblique arc-continent collision. Preliminary results are presented in this poster

This research is part of project PGC2018-094227-B-I00 funded by the Spanish Research Agency from the Ministry of Science Innovation and Universities of Spain. JA is funded by MICINN (Juan de la Cierva fellowship - IJC2018-036074-I).

19th International Symposium on Deep Seismic Profiling of the Continents and their Margins, 15th – 20 th March 2020, Perth, Australia

Country

Spain

Related Organizations

Spanish National Research Council
Spain

Keywords

Taiwan

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