Titlebook: Backarc Basins; Tectonics and Magmat Brian Taylor Book 1995 Springer Science+Business Media New York 1995 evolution.geology.sediment.sedime

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Etienne de Klerk,Tamás Terlaky,Kees Roosone. Melt preferentially rises through the fissures and faults created by extension in the continental crust. The total amount of extension across the Okinawa Trough has been estimated from refraction and gravity data. It decreases slightly from 80 km in the southern Okinawa Trough to 74 km in the n

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Russell J. McCulloh M.D.,Steven M. Opal M.D.s understandable because of small differences in parameters, such as magma signature and composition of oceanic crust, between those two systems. Frontal-arc volcanoes are proved to be the sites of vigorous high-temperature hydrothermal activity. Several investigated submarine calderas in the Izu-Bo

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Marcel Levi M.D., Ph.D., F.R.C.P. black glassy volcanic fragments within coarse, sandy intervals associated with these arc systems suggest that the early rift phase of backarc basin formation is characterized by felsic (bimodal) volcanism and that volcanic centers become progressively more intermediate with time. This trend is cons