関連する実験動画

Updated: May 12, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 16, 2013

エクロジットの部分的な溶解による初期の大陸地殻の成長

Robert P Rapp1, Nobumichi Shimizu, Marc D Norman

  • 1Mineral Physics Institute and Department of Geosciences, State University of New York at Stony Brook, Stony Brook, New York 11794-2100, USA. rrapp@notes.cc.sunysb.edu

Nature
|October 10, 2003
PubMed
まとめ

実験的証拠は,初期の地球弧マグマティズムがトナライト・トンドヘミト・グラノディオライト (TTG) 岩を産んだことを示しています. エクロジット面における水性玄武岩の部分的な溶解により,TTG液体が生成され,海内島が初期の大陸地殻形成の鍵であったことを示唆しています.

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