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Updated: Jul 26, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

MELT領域内の東太平洋の上昇と沿いに軸外地殻の厚さが上昇する

Canales1, Detrick, Bazin

  • 1J. P. Canales and R. S. Detrick, Department of Geology and Geophysics, Woods Hole Oceanographic Institution, 360 Woods Hole Road, Woods Hole, MA 02543, USA. S. Bazin, A. J. Harding, J. A. Orcutt, Institute of Geophysics and Planetary.

Science (New York, N.Y.)
|June 5, 1998
PubMed
まとめ

ナスカ・プレートと太平洋プレートは,類似した地殻の厚さを示しており,東太平洋の上昇における深さと重力の変動とは異なる. これらの違いは,地殻の年齢ではなく,マントルの密度の変動から生じる可能性が高い.

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