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Cenozoic continental arc magmatism and associated mineralization in Ecuador

✍ Scribed by Massimo Chiaradia; Lluís Fontboté; Bernardo Beate


Book ID
105822690
Publisher
Springer
Year
2004
Tongue
English
Weight
847 KB
Volume
39
Category
Article
ISSN
0026-4598

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The Okinawa Trough is a young, intracontinental backarc basin that has formed behind the Ryukyu arc–trench system since late Miocene time. In the Southernmost Part of the Okinawa Trough (SPOT), a cluster of active submarine volcanoes delineates a volcanic belt, which is located only ∼100 km above th