南東太平洋の下のマントルの不連続構造は,PからSに変換された相から上昇します
1Y. Shen, Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. A. F. Sheehan, K. G. Dueker, H. Gilbert, Cooperative Institute for Research in Environmental Sciences (CIRES), University of.
まとめ
地震受容器の機能は,南東太平洋上昇の下にあるマントルの正常な移行ゾーンの厚さを明らかにします. これは,マントルの移行ゾーンで余分な熱を伴う上流が存在しないことを示唆しています.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地震学 地震学とは
- 地球科学 地球科学 地球科学
背景:
- マントルの移行領域 (MTZ) は,マントルの動態を理解するための重要な領域です.
- 海底の地震計は,地球の深層構造の地震イメージングに不可欠なデータを提供します.
研究 の 目的:
- 南東太平洋上昇線の下にあるMTZの構造と熱状態を調査する.
- マントルの上流が異常なMTZ特性と関連しているかどうかを判断する.
主な方法:
- テレシーミックボディ波からの受信機能の分析.
- 海底の地震計を使用して地震データを記録する.
- マントルの不連続性 (410kmと660kmの深さ) で切断波変換を特定する.
主要な成果:
- 南部東太平洋上昇の下にあるMTZの厚さは,世界の平均と一致しています.
- より浅いまたはより厚いMTZの証拠は見つかりませんでした.
結論:
- 南部東太平洋上昇の下の上流は,MTZの過度な温度と関連しているようには見えない.
- この地域の下にあるMTZは正常な地震特性を示しており,重大な熱異常がないことを示している.
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