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Updated: Aug 6, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

アークマグマのU-Thイソトープ: 吸収された地殻からの元素移転への影響

Hawkesworth1, Turner, McDermott

  • 1C. J. Hawkesworth, S. P. Turner, D. W. Peate, and P. van Calsteren are with the Department of Earth Sciences, The Open University, Milton Keynes, MK7 6AA, UK. F. McDermott is with the Department of Geology, University College, Dublin, Eire.

Science (New York, N.Y.)
|April 25, 1997
PubMed
まとめ

ウラン・ソリウム・イソトープは,流体と沈殿物の流出速度を,地質プレートからの流出速度を示している. 島弧の火山岩は,流体がウランを動員していることを示しており,堆積物は弧岩のトリウムに大きく貢献しています.

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