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地球の石層マントルの融解は,プロタクトニウム・ソリウム・ウランの同位体データから推測される

Asmerom1, Cheng, Thomas

  • 1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque 87131, USA. asmerom@unm.edu

Nature
|August 5, 2000
PubMed
まとめ

科学者たちは,大陸の玄武岩から得られたウラン・ソリウム・プロタクトニウム同位体データを用いて,石層マントルの融解を理解した. この研究は,溶けた小さな分子が,石層を素早く移動する方法を明らかにしています.

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