[S-IT04] Rheology of Earth's Interior

[SIT04-05] 島弧の沈み込み量の推定

*市川 浩樹¹、河合 研志²、山本 伸次²、亀山 真典¹ (1.愛媛大学　地球深部ダイナミクス研究センター、2.東京大学　総合文化研究科)

キーワード：大陸地殻, 島弧, マントル, 沈み込み, レオロジー

Evolution of life on the Earth is strongly related to the oceans and the continents, both of which are unique to the Earth. Continental materials contain a large amount of incompatible and radiogenic elements, which may affect terrestrial thermal history and chemical evolution, as well as the Earth's surface environment. Geological studies have revealed that continental materials subduct from the Earth's surface via the following three mechanisms: tectonic erosion, sediment subduction, and direct subduction of immature oceanic arcs, which are found, for example, in the western Pacific. In the first two processes, the continental materials are conveyed through subduction channels of thickness of 2-3km just above the subducting slabs. Here, in order to estimate the supply rate of continental materials of oceanic arcs to the deep mantle, we have conducted numerical simulations of subduction of arcs based on the finite element method, using relevant rheology models. The results show that the subduction rate highly depends on temperature profiles of the subducting slabs and the size of the arcs.