The study of multi‐isotope systematics of fluid inclusions is of great importance for understanding of the sources and evolution of fluid phase in mantle rocks and ore deposits. The most appropriate technique for such investigations is (stepwise) crushing method that is widely used for noble gases and nitrogen. However because of possible influence of mechanochemical reactions and back sorption, analyses of isotope composition of water extracted by crushing from fluid inclusions are challenging.

中文翻译：

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基于同位素比率质谱法的亚微升水中氢同位素分析方法：从流体包裹体中提取气体的多同位素研究中的应用。

流体包裹体的多同位素体系研究对于理解地幔岩石和矿床中流体相的来源和演化具有重要意义。最适合此类研究的技术是（逐步）破碎法，该方法广泛用于稀有气体和氮气。但是，由于机械化学反应和反吸附的可能影响，分析通过压碎从流体包裹体中提取的水的同位素组成具有挑战性。