Crustal and basin evolution of the southwestern Barents Sea: From Caledonian orogeny to continental breakup
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Active continental subduction and crustal exhumation: the Taiwan orogeny
It is generally accepted that continental subduction and crustal exhumation play an important role in the evolution of many orogenic belts. A variety of geological evidence suggests that continental crust is occasionally subducted to depths of tens to perhaps 150 km (e.g. Chopin, 1984; Dewey et al., 1993; Matte et al., 1997). Recently, a series of simulations (Chemenda, 1993; Chemenda et al., 1...
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ژورنال
عنوان ژورنال: Tectonics
سال: 2014
ISSN: 0278-7407
DOI: 10.1002/2013tc003439