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Updated: Jun 25, 2026

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High Pressure Single Crystal Diffraction at PX^2
Published on: January 16, 2017
クリノエンスタチトがアルペアラムイ・ペリドートに含まれる:非常に高い圧力の追加証拠
Bozhilov1, Green, Dobrzhinetskaya
1Institute of Geophysics and Planetary Physics and Department of Earth Sciences, University of California, Riverside, CA 92521, USA.
まとめ
トランスミッション電子顕微鏡では,スイスアルプスのガーネット・ヘルゾライトのクリノエンスタチット・ラメラが発見された. これらの発見は,大陸の衝突の前に少なくとも250kmから深い岩の発掘を示唆しています.
科学分野:
- ミネラロジーとペトロロジー
- 地質化学 地質化学
- テクトニクス (地質学) とは
背景:
- ガーネット・ヘルゾライトは,地球の上層マントルの組成と条件についての洞察を提供します.
- 鉱物溶解のラメラの理解は,地質の歴史を再構築するのに役立ちます.
- アルペ・アラミ山脈は,マントルのクセノリフを研究するための重要な地域である.
研究 の 目的:
- ディオプシド粒子の内にあるクリノエンスタチトのラメラの微細構造と結晶学を調査する.
- 溶解過程を解釈し,宿主岩のP-T条件を推論する.
- アルペ・アラミ・ガーネット・ヘルゾライトの発掘の深さを決定するために.
主な方法:
- トランスミッション電子顕微鏡 (TEM) は,鉱物の微細構造の高解像度イメージングに使用されました.
- 溶解後のラメラの結晶学分析.
- ディオプサイド-クリノエンスタチト系内の相関係分析.
主要な成果:
- クリノエンスタチトのラメラは,アルペ・アラミのガーネット・ヘルゾライトのダイオプシド粒子の内部で特定されました.
- オリエンテーション,結晶学,および微細構造は,高圧C中心のクリノエンスタチート相からの溶解と一致しています.
- 相関係分析は,この解釈を裏付けている.
結論:
- C中心のクリノエンスタチトの溶解は,高圧で形成されたことを示している.
- これらのラメラの存在は,岩石が少なくとも250キロメートルの深さから発掘されたことを示唆しています.
- この発掘の出来事は,大陸の衝突の前に,またはその間に起こった可能性が高い.
関連する概念動画
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When a rod is under axial loading, the internal forces and corresponding stress are normal to the plane of the section, so it is termed normal stress. It's important to...
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The shearing force, possessing potential directionality within the plane of the section, is simplified into two component forces running parallel to the x and y axes.
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