Late Cretaceous–Paleocene evolution of the East Gondwana margin, a new dynamic model for the formation of marginal basins
Late Cretaceous–Paleocene evolution of the east Gondwana margin Plate reconstructions in a mantle reference frame show that from 140 to 105 Ma Gondwana moved eastward toward the Pacifi c Plate. This convergence was largely accommodated by the subduction of the Pacifi c Plate under Gondwana. Between...
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Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.6209 http://www.earthbyte.org/people/dietmar/Pdf/Rey_Muller_East_Gondwana_margin_evolution_EABS2008.pdf |