チベットの熱くて乾燥した深層地殻のキセノリフ
1Geological Sciences, University of California, Santa Barbara, CA 93106, USA. Mineralogisch-Petrographisches Institut, University of Bern, Baltzerstrasse 1, CH-3012 Bern, Switzerland. Institut fur Geologie, Technische Universitat Bergakademie.
まとめ
チベット高原はチベット高原です.
科学分野:
- 地質学 地質学 地質学
- 地質物理学 地質物理学とは地質物理学です.
- ペトロロジー・ペトロロジーとは
背景:
- チベット高原の中央部のショショニット岩層には,キセノリトが含まれています.
- これらのクセノライトは,地殻の深い状態についての洞察を提供します.
研究 の 目的:
- チベット高原の中央部の地殻の熱条件と融解過程を調査する.
- 広範囲にわたる地殻の融解が起きているかどうかを判断する.
主な方法:
- 無水性メタセデミントおよびマフィック・キセノリトの分析.
- P波の速度とプアソン比率の計算.
- 計算された地震特性と地震学的観測を比較する.
主要な成果:
- エクセノライトは,深さ30~50kmで800~1000°Cの熱グラデントを示している.
- エクセノリフの採取前加熱は200°Cまで達した.
- 水性ミネラルの欠如と地震データは,広範囲にわたる地殻の融解と矛盾しています.
結論:
- チベットの中央の地殻は,ミカの脱水溶解に十分な温度です.
- 地震データと鉱物学は,地殻の溶解が限られたか,全くなかったことを示唆している.
- 深層地殻の熱状態と融解プロセスは複雑である.
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