https://doi.org/10.15407/gpimo2016.02.037
Geology and Mineral Resources of World Ocean 2016, 12 (2): 37-47
V.V. Gordienko, L.Ya. Gordienko
Institute of Geophysics of NAS of Ukraine, Kyiv
A VELOCITY MODEL FOR BACKARC BASINS UPPER MANTLE
According to the arrival time of the Pwaves from earthquakes beneath backarcs basins of Pacific hodographs are built at distances up to 25 degrees. It is allowed to establish the speed distribution up to depths of about 450—500 km. It is established the low velocity zone in the upper mantle from 80 to 150 km, where the partial melting of the rocks is probably. The geologic history and deep processes in backarc basins are analyzed. It is stablished that endogenous oceanization condition is inherent in them.
Key words: back-arcs basins, velocity sections, oceanization.
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