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Updated: Jul 10, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 15, 2013

地球の深い上層マントルの融解は,二酸化炭素によるものです

Rajdeep Dasgupta1, Marc M Hirschmann

  • 1Department of Geology and Geophysics, University of Minnesota, 310 Pillsbury Drive SE, Minneapolis, Minnesota 55455, USA. dasg0007@umn.edu

Nature
|March 31, 2006
PubMed
まとめ

炭酸ペリドータイトによって引き起こされる中海の山脊の下の部分的な融解は,以前考えられていたよりも深く起こります. このプロセスは元素の循環とマントルの性質に影響を与え,地球に影響を与えます.

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Dynamic Pore-scale Reservoir-condition Imaging of Reaction in Carbonates Using Synchrotron Fast Tomography

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Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.07:32

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.

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