デッカンの罠の深層マントルの起源について
Petar Glišović1, Alessandro M Forte2,3
1GEOTOP, Université du Québec à Montréal, Montréal, Québec H3C 3P8, Canada. glisovic.petar@uqam.ca.
まとめ
デッカン・トラップス噴火は,レユニオン島とコモールのホットスポットの下の深いマントルの羽根と関連付けられました. この研究は,洪水ベースルトの出来事を理解するために,初期のケノゾイクマントルの構造を再構築します.
科学分野:
- 地理学
- 地力学
- 地球科学
背景:
- デッカン・トラップは 地球最大の大陸の 岩地帯の"つです
- その噴火は白亜紀・旧亜紀の絶滅に 関わっている.
- インド洋の下の初期のケノゾイクマントルの構造はよくわかっていないため,深層マントルの起源の接続を妨げている.
研究 の 目的:
- ケノゾイク初期におけるマントルの構造を再構築する.
- デッカン・トラップス噴火の 深いマントルの起源を調査するために
主な方法:
- タイム・リバースド・コンベクション・モデリングの反復的な方法を使用した.
- トモグラフィーに基づく,現在のマントルの異質性データ.
主要な成果:
- デッカンの噴火と一致する 熱いスポットの下の 低密度の噴出を特定した
- コモール熱点の下の 第二の活発な上昇を検知した 噴火のマグマ源に寄与している可能性が高い
結論:
- デカン・トラップス噴火は,レユニオン島とコモール島の両方のホットスポットから生じた深いマントルの羽根によって引き起こされました.
- 大規模なバサルトの洪水と 大量絶滅における潜在的役割との深いマントルのつながりを提供します
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