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Updated: Jul 13, 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

マグマガス組成は,スラグ駆動ストロンボリアン爆発活動の源の深さを明らかにします

Mike Burton1, Patrick Allard, Filippo Muré

  • 1Istituto Nazionale di Geofisica e Vulcanologia, Catania, Italy. burton@ct.ingv.it

Science (New York, N.Y.)
|July 14, 2007
PubMed
まとめ

ストロンボリアン噴火を誘発するガスのスランプは,火山と地殻のインターフェースの奥深く,約3キロメートルの深さで形成されます. この深い起源は,ストロンボリ火山で観測されたスラグ形成と浅い爆発地震の間の断絶を説明しています.

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