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

Incorporate

Venkataramanan Balakrishnan,Fan Wangs are summarized on the basis of updated geophysical and geological data, including swath bathymetry, gravity, magnetics, and seismic reflection profiling records as well as results from the DSDP/ODP drilling holes. It has been proposed that the Shikoku Basin was born as a rift separating the N-S tr

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W. Joost Wiersinga,Christopher W. Seymourhich is 7–8 km deep, and it contains 4 to 5+ km of technically undisturbed sedimentary fill. The oldest sedimentary rocks sampled from the basin margin are Miocene/Oligocene. Although no seafloor spreading magnetic lineations exist, we conclude that the basin has formed by backarc extension and spre

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Russell J. McCulloh M.D.,Steven M. Opal M.D.luid chemistry. These sites constitute about 20% of the known seafloor hydrothermal sites, which are dominated by those occurring at mid-ocean ridges (MORs). High-temperature hydrothermal activities in the western Pacific exclusively occur in association with submarine volcanism found either on back

BROTH

Marcel Levi M.D., Ph.D., F.R.C.P.axis. These models are adequate in the case of backarc rifting, but a more dynamic model is needed in the case of forearc rifting. We present a revised model for backarc basin sedimentation that reflects progressive shifts in volcanism and associated depocenters through the history of a backarc basi

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Book 1995ano-tectonicprocesses are best studied because of their activity. Key themes inthis volume include volcano-tectonics setting; cause and location;rift magmas; and hydrothermal activity. Researchers also presentmodels of the dynamic processes occurring in backarc basins.

COLIC

where volcano-tectonicprocesses are best studied because of their activity. Key themes inthis volume include volcano-tectonics setting; cause and location;rift magmas; and hydrothermal activity. Researchers also presentmodels of the dynamic processes occurring in backarc basins.978-1-4613-5747-6978-1-4615-1843-3

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e to mature spreading. Complete with numerousillustrations, each of the twelve chapters focuses on a young, activebackarc basin of the circum-Pacific-where volcano-tectonicprocesses are best studied because of their activity. Key themes inthis volume include volcano-tectonics setting; cause and loca