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Simulation of the Planetary Interior Differentiation Processes in the Laboratory
Published on: November 15, 2013
地球科学:湿ったマントルの導体?
1Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA. marc.m.hirschmann-1@umn.edu
Nature
|January 27, 2006
まとめ
地球のマントルの移行地帯は,以前考えられていたほど多くの水を保持していないかもしれません. 水分含有量が高くなく,条件の減少が,おそらくその電気伝導性を説明し,地動力学と地化学に影響を与えます.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地質化学 地質化学
- ミネラル物理学 ミネラル物理学
背景:
- 地球のマントルの移行地帯 (深さ410~670km) は,マントルの動力学と地球規模の水循環にとって極めて重要です.
- 以前の研究では,電気伝導性に基づいて,このゾーンで水分が著しく濃縮されていることが示唆されていました.
- この解釈は,移行地帯内の酸化状態の仮定に基づいていた.
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