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Alternative magmatic processes of continental growth in an island arc

✍ Scribed by Eichhorn, M.


Book ID
121957006
Publisher
Elsevier Science
Year
1981
Weight
87 KB
Volume
28
Category
Article
ISSN
0198-0254

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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