アメリカ合衆国セントヘレンズ山の火山活動の地化学的前駆体
Kim Berlo1, Jon Blundy, Simon Turner
1Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Rd, Bristol BS8 1RJ, United Kingdom. Kim.Berlo@bristol.ac.uk
まとめ
セントヘレンズ山の噴火前の脱ガスと結晶化プロセスが噴火のスタイルに影響を与えた. マグマの地化学的シグネチャは,数十年から数日の脱ガス状態を明らかにし,マグマの停滞と揮発性蓄積を示しています.
科学分野:
- 火山学 火山学とは
- 地質化学 地質化学
背景:
- マグマの脱ガス化と結晶化の相互作用は,火山噴火の理解に極めて重要です.
- 以前の研究では,1980年のセントヘレンズ山噴火におけるこれらのプロセスの重要性を確立しました.
研究 の 目的:
- 火山噴火前のマグマ脱ガス化のタイミングと特性を調査する.
- 地化学データを用いて,脱ガスパターンと噴火スタイルを相関させる.
主な方法:
- 微量元素の分析,特にリチウム.
- 短命放射性同位体,鉛-210およびラジウム-226.6を含む短命放射性同位体の測定
- マグマ内の地化学的シグネチャの解釈.
主要な成果:
- 脱ガス化は,噴火の前数十年から数日までの長期間,発生しました.
- 地化学的なシグネチャは,マグマが火山の管内に停滞したことを示しています.
- この停滞は,揮発性の蓄積と鉛-210の過剰の形成につながり,深いところでの脱ガスにシグナルを与えました.
結論:
- 脱ガスパターンは,セントヘレンズ山の噴火様式を示しています.
- マグマの停滞と揮発性物質の蓄積は,噴火に先立つ重要なプロセスである.
- 鉛-210の過剰は,マグマの脱ガス化のための地化学マーカーとして機能します.
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