まとめ
メタモルフィック・ガーネットにおける酸素同位体のゾーニングは,メタモルフィズム中の流体浸透と脱水反応を明らかにする. 酸素同位体値 (デルタ{18) O) のこれらの変化は,地質学的過程の洞察を提供します.
科学分野:
- 地質化学 地質化学
- 同位体地質学とは,同位体地質学である.
- メタモルフ Petrology メタモルフペトロロジー
背景:
- ガーネットは,変形岩の重要な鉱物であり,P-T条件に関する情報を保存しています.
- 酸素同位体分析は,流体と岩の相互作用を追跡するための強力なツールです.
研究 の 目的:
- メタモルフィック・ガーネット内の酸素イソトープのゾーニングを調査するために.
- 石榴石の地化学に対する変異過程の影響を理解するために.
主な方法:
- 酸素同位体 (デルタ) の安定同位体レーザー探査分析 (O).
- ヴァーモント州とユタ州の4つの石榴石の調査.
主要な成果:
- 濃縮酸素同位体ゾーニング (デルタ(18) O) は,すべての調査されたガーネットで観察されました.
- 地域的な変形石榴石は,最大の変動を示した (コアからリムまで1ミリあたり3まで).
結論:
- ガーネットの酸素同位体の区分は,成長中の岩のデルタの変化を反映しています.
- 液体の浸透と脱水反応は,変異過程におけるこれらの同位体変化の主要な原動力である.
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