1980年5月18日にモスクワ・プルマン地区にあるセントヘレンズ山の灰の構成
まとめ
1980年5月18日に発生したセントヘレンズ山の火山灰は,2つの異なる灰の種類で構成されています. 鉱物学的および化学的分析により,初期のダークアッシュと後の淡いアッシュの間の大きな違いが明らかになった.
科学分野:
- 地質化学 地質化学
- ミネラロジーは,鉱物学です.
- 火山学 火山学とは
背景:
- 1980年のセントヘレンス山の噴火は,大量の灰を降ろした.
- 火山灰の組成を理解することは,その影響を評価するために不可欠です.
研究 の 目的:
- 1980年5月18日の噴火で発生した灰の詳細な鉱物学および化学分析を行う.
- 堆積した異なる灰の種類を区分し,特徴づけること.
主な方法:
- 灰塵のサンプルを鉱物学的に分析する.
- 灰分とガラスの部品の化学分析.
- 鉱物相と元素組成の識別.
主要な成果:
- 2つの異なる灰のタイプが特定されました:初期の暗い灰と後の淡い灰です.
- 濃い灰にはプラジオクラゼ,リチック断片,マグネチット,ホーンブレンド,オルトピロキセンが含まれていた.
- 淡い灰は主にガラス (80%) で,プラジオクラスが主要な結晶相であり,クォーツとカリウムフェルドスパートが稀であった.
結論:
- 鉱物学的および化学的なデータは,セントヘレンズ山噴火からの2種類の異なる灰の存在を確認しています.
- 分析により,初期の灰堆積と後の灰堆積の組成の有意な違いが明らかになった.
- 両方の灰型は,それぞれの分数の内部で化学的同質性を示した.
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