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- W2364110631 abstract "Thermal parameters have been calculated for different temperature and pressure. The results have been compared with the results of other authors. The evolution of the thermal regime of Japan Sea subduction zone has been calculated by the Finite Element Method (FEM). It was found that the isothermal line of 400℃ is being at stable after subducting 7 Ma, its deepest depth is about 60 km; the isothermal line of 800℃ is being at stable after subducting 11 Ma, its deepest depth is about 280 km; and the isothermal line of 1200C is being at stable after subducting 50 Ma, its deepest depth is about 530 km. Through calculating the thermal structure of Japan Sea subduction zone at different heat sources assembly, we have discussed the effect of the heat sources to the thermal structure of the subduction zone. The resuls showed that the shear strain heating and the dehydration heating affect greatly the thermal regime of the shallow region; adiabatic heating has effect at the most vast region; Olivine-Spinel phase change heating is the controlling factor of the thermal regime of the region deper than 400 km." @default.
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- W2364110631 date "1993-10-17" @default.
- W2364110631 modified "2023-09-22" @default.
- W2364110631 title "ON THE THERMAL STRUCTURE OF THE JAPAN SEA SUBDUCTION ZONE AND THE EFFECT OF THE HEAT SOURCES" @default.
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