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Updated: Jun 16, 2026

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

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オリヴィンとクロミットにおける元素拡散による異常な溶融インクルージョンの生存時間

C Spandler1, H St C O'Neill, V S Kamenetsky

  • 1Research School of Earth Sciences, Australian National University, Canberra 0200, Australia. spandler@geo.unibe.ch

Nature
|May 18, 2007
PubMed
まとめ

オリヴィンとクロミットの溶融含有物は,初期のマントルの溶融組成物を保存しません. 稀土元素の急速な拡散は,マグマの温度で,噴火前のインクルージョンのバランスをとります.

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