プレカンブリアプレート構造におけるクラトニックキールの構築
A L Perchuk1,2, T V Gerya3, V S Zakharov4
1Geological Faculty, Lomonosov Moscow State University, Moscow, Russia. alp@geol.msu.ru.
Nature
|October 15, 2020
まとめ
古代の大陸のコア (クラトン) は,プレカンブリアの沈殿によって形成された深いマントルのキールを特徴としています. この過程で厚く層状の石層が形成され クラトン生存とダイヤモンドの形成に 重要な役割を果たしました
科学分野:
- 地質学
- 地理学
- 構造学
背景:
- 厚いマントルのキールを持つ 古代の大陸の核です
- マントルキールは,隔離され,枯渇し,浮遊し,ダイヤモンドを含むマントル体積です.
- キールの形成は初期地球 (1.5~35億年前) にのみ発生し,現代的な類似点がない.
研究 の 目的:
- マントルキールの起源を調査する
- 初期の地質学がキール形成に 果たした役割を調べる
- クラトン長寿の条件を理解する
主な方法:
- 海洋沈殿と大陸の衝突をモデル化しました
- 地球マントルの初期温度 (150~250°C以上) の上昇をシミュレートした.
- プロトケールの位置と冷却の動態を分析した.
主要な成果:
- 熱い浮遊する亜石層マントルは 沈殿板の下では沈殿しなかった.
- クラトン規模のプロトケールが 置き去りにされた
- プロトケール厚さは,クレートン石層の年齢最大値と相関する.
結論:
- プレカンブリア時代には 枯渇した海洋プレートが 層状のマントルキールを形成した.
- このメカニズムはキール層とクレートンの生存を説明します
- その後のプロトケルの冷却により ダイヤモンドが形成された.
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