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Reactivation of Inherited Oblique Continental Margin Structures During the Development of the South-Central Taiwan Fold and Thrust Belt

AutorBiete, Cristina ; Alvarez-Marrón, Joaquina ; Brown, Dennis ; Kuochen, H.; Ho, Chun-Wei; Wu, Y. M.
Fecha de publicación12-dic-2016
ResumenThe Taiwan orogen is forming due to the oblique collision between the Eurasian continental margin and the Luzon Arc. This configuration provides an opportunity to study the effect of inherited structures on the development of a fold and thrust belt (FTB). During the extensional tectonic history of the margin several NE trending basins filled with Eocene to Early Oligocene sediments developed on a pre-­‐Cenozoic basement, and further extension took place on the outer margin during the Middle to Late Miocene. The margintransition from the platform to the slope, and the large-­‐scale extensional features of the margin project obliquely onland across south-­‐central Taiwan. These basins are now involved in the Taiwan FTB.
URIhttp://hdl.handle.net/10261/163828
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