弧火山の位置に関するグローバル・システマティック.
Philip C England1, Richard F Katz
1Department of Earth Sciences, Parks Road, Oxford OX1 3PR, UK. philip.england@earth.ox.ac.uk
Nature
|December 15, 2010
まとめ
サブデュークションゾーン上の火山の弧の位置は,クロライトの安定性限界によって説明されません. 数値モデルのエラーと偽の相関は,マントルの融解プロセスに関する以前の結論を無効にします.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- ペトロロジー・ペトロロジーとは
- テクトニクス (地質学) とは
背景:
- サブダクションゾーン上の火山弧の位置は,従来,サブダクションスラブから水性流体の放出によって引き起こされるマントルの融解プロセスと関連しています.
- 以前の研究では,弧火山が特定の温度と鉱物の安定性,特に塩素酸塩の安定性内のマントルの融解によって制御されることを提案しました.
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