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- W4205451131 abstract "Abstract The thermal structure of the Japan island arc, one of the most active parts of volcanism, occupying over 10 percent of the worldwide volcanoes, remains an enduring problem. The key to understanding geothermal development is estimating the temperature distribution in the deep crustal depth of island arcs. This study extracts the temperature component from deep crustal seismic tomography. The deep crustal temperature map shows that the deep crustal high-temperature zone along the volcanic front (the Ou Backbone Mountains) and the high-temperature parts extend towards the Quaternary volcanos in the west, which corresponds to the hot finger model. The deep crustal high-temperature part also exists around Iide mountain, where no Quaternary volcanoes exist. The high-temperature part without volcanic activity suggests heat transfer due to high-temperature fluid from the mantle. A deep crustal low-temperature zone develops along the Miocene rift around the eastern margin of the Japan Sea. The low temperature probably reflects the small heat generation due to the small amount of radioactive elements in the mafic crust." @default.
- W4205451131 created "2022-01-26" @default.
- W4205451131 creator A5001727346 @default.
- W4205451131 date "2022-01-17" @default.
- W4205451131 modified "2023-10-17" @default.
- W4205451131 title "Thermal structure of the island arc crust, northeast Japan" @default.
- W4205451131 doi "https://doi.org/10.21203/rs.3.rs-1222111/v1" @default.
- W4205451131 hasPublicationYear "2022" @default.
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