ロングバレーのカルデラの下にあるマグマの侵入は,重力の時間的な変化によって確認されています
1Department of Geophysics, Stanford University, Stanford, CA 94305, USA. U.S. Geological Survey, Menlo Park, CA 94025, USA.
まとめ
カリフォルニア州ロングバレーの重力測定では,マグマの侵入を示唆する大幅な減少が示されています. この発見は,上昇と地震活動の原因として,熱膨張や熱水圧を排除しています.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 火山学 火山学とは
背景:
- カリフォルニア州ロングバレー・カルデラは,表面の上昇と地震性を示しています.
- 以前の研究では,熱膨張と熱水活動を含むこれらの現象の様々な原因が示唆されました.
研究 の 目的:
- ロングバレー・カルデラの上昇と地震性を推進する地下過程を調査する.
- 重力の変化に起因する侵入物質の性質を決定する.
主な方法:
- 精密な相対重力の測定は,1982年と1998年に行われました.
- 重力データを分析して変化を検出し,上昇と表水位変動などの既知の効果を修正しました.
主要な成果:
- 復活したドームを中心に -107 +/- 6 マイクロガルまでの重力の減少が観察されました.
- 修正後,最大64 +/- 15マイクロガルまでのポジティブな残留重力変化が検出されました.
- 侵入物質の密度は2.7×10^3から4.1×10^3kg/m^3.3の間で推定された.
結論:
- 重力データは,上昇と地震の原因としてシリケートマグマの侵入を強く支持しています.
- 主要な要因として,インシット熱膨張や水熱システム圧縮は除外される.
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