日本地球惑星科学連合2015年大会

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セッション記号 S (固体地球科学) » S-IT 地球内部科学・地球惑星テクトニクス

[S-IT35] 地球深部ダイナミクス:プレート・マントル・核の相互作用

2015年5月26日(火) 16:15 〜 18:00 106 (1F)

コンビーナ:*中川 貴司(海洋研究開発機構数理科学・先端技術研究分野)、綿田 辰吾(東京大学地震研究所海半球観測研究センター)、境 毅(愛媛大学地球深部ダイナミクス研究センター)、座長:古市 幹人(海洋研究開発機構)、境 毅(愛媛大学地球深部ダイナミクス研究センター)

16:15 〜 16:30

[SIT35-07] 生命居住惑星とプレートテクトニクスの役割

*丸山 茂徳1 (1.東京工業大学地球生命研究所)

Plate tectonics plays a role of global material circulation from the surface of the earth to the bottom of mantle since ca.4.0Ga. This is a due function both to bear habitable planet and to evolve as a habitable planet.
In spite of empirical recognition of importance of plate tectonics, nobody succeeded to synthesize the role of plate tectonics. However, the author completed this task by using following data; (1) geophysical constraints for the mechanism of plate tectonics, (2) petrological and geochemical characteristics of lithosphere, and (3) geologic history of the Earth, specifically the structural and petrological remarks of rock components and dynamics recorded in orogenic belts over the world.
As the result, basic condition for the operation of plate tectonics and following 6 roles of plate tectonics were summarized. The reason why plate tectonics is operated on the Earth is because mid-oceanic ridge is hydrated to enable plate to subduct which is helped by the lubricant water-rich fluids on the bottom of lithosphere. Roles of plate tectonics are (1) Global material circulation of CO2 and H2O, (2) Role of tectonic erosion, (3) Production of nutrients-source rocks at subduction zone, (4) Driving force of Earth's magnetic filed, (5) The buffer of Earth's system, and (6) The controller of thermal history of the Earth.