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Updated: Jan 10, 2026

Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment
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キンベルライトの上昇は,同化燃料による浮力によるものです

James K Russell1, Lucy A Porritt, Yan Lavallée

  • 1Volcanology and Petrology Laboratory, Earth and Ocean Sciences, University of British Columbia, Vancouver V6T 1Z4, Canada. krussell@eos.ubc.ca

Nature
|January 20, 2012
PubMed
まとめ

キンベルライトのマグマは,カルボナイトのような溶液がマントルのミネラルを同化し,揮発性の溶解を引き起こす新しいメカニズムにより急速に上昇します. このプロセスは,それらの深い起源,高速,そしてダイヤモンドを含む密度の高いキセノリットを運ぶ能力を説明します.

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