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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Combined microthermometric and Raman spectroscopic technique to determine the salinity of H_2O-CO_2-NaCl fluid inclusions based on clathrate melting
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Combined microthermometric and Raman spectroscopic technique to determine the salinity of H_2O-CO_2-NaCl fluid inclusions based on clathrate melting

机译:结合体温和拉曼光谱技术确定基于包合物熔融的H_2O-CO_2-NaCl流体包裹体的盐度

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Fluid inclusions approximated by the system H_2O-CO_2-NaCl are common in many geologic environments. In order to apply microthermometric data from these inclusions to infer P-T (pressure-temperature) trapping conditions, the composition of the inclusions, including the salinity, must be known. Normally, salinities of aqueous inclusions are determined from ice-melting temperatures obtained during microthermometry. However, when CO_2-bearing aqueous fluid inclusions are cooled they often form a hydrate that incorporates H_2O into the structure, and salinities estimated from ice-melting temperatures are therefore higher than the actual salinity. A technique that combines data from Raman spectroscopic and microthermometric analyses of individual inclusions was developed to determine the salinity of CO_2-bearing aqueous inclusions based on measured clathrate melting temperatures and CO_2 pressures obtained from Raman analyses. In this study, the pressure within inclusions was determined using Raman spectroscopy based on the splitting of the Fermi diad of CO_2, measured at the clathrate melting temperature. The CO_2 densities (and pressures) predicted by the equation developed in this study are in relatively good agreement with previously published equations, except for very low densities and correspondingly low pressures. The combined Raman spectroscopy - microthermometry technique thus provides both the temperature and the pressure in the inclusion at clathrate melting. For inclusions in which the clathrate melts in the presence of CO_2 liquid, the salinity can be determined with a precision of a few tenths of a wt% NaCl, whereas for inclusions in which clathrate melts in the presence of CO_2 vapor the salinity error may be a few wt% NaCl. Applying the method to synthetic fluid inclusions with known salinity suggests that the technique is valid for determining salinity of H_2O-CO_2-NaCl fluid inclusions in which clathrate melts in the presence of liquid CO_2 only or vapor CO_2 only.
机译:由H_2O-CO_2-NaCl系统近似的流体包裹体在许多地质环境中都很常见。为了将来自这些夹杂物的微热数据应用于推断P-T(压力-温度)捕获条件,必须知道夹杂物的组成,包括盐度。通常,含水夹杂物的盐度由在微量热测定法中获得的融冰温度确定。但是,当冷却含CO_2的含水流体夹杂物时,它们通常会形成将H_2O掺入结构的水合物,因此从冰融化温度估算的盐度高于实际盐度。开发了一种技术,该技术结合了来自拉曼光谱和单个夹杂物的显微热分析的数据,可根据测得的包合物熔融温度和从拉曼分析获得的CO_2压力,确定含CO_2的含水夹杂物的盐度。在这项研究中,夹杂物内的压力是使用拉曼光谱法基于在包合物熔融温度下测量的CO_2费米二元分解的结果确定的。通过本研究开发的方程式预测的CO_2密度(和压力)与以前发表的方程式相对较好,除了非常低的密度和相应的低压力。因此,结合的拉曼光谱-微热技术可以在包合物熔融时提供夹杂物的温度和压力。对于包合物在CO_2液体存在下熔化的夹杂物,其盐度可以精确到十分之一重量百分比的NaCl来确定,而对于包合物在CO_2蒸气存在下熔化的夹杂物,其盐度误差可能是少量的氯化钠。将该方法应用于盐度已知的合成流体包裹体,表明该技术对于确定仅在液态CO_2或仅在蒸气CO_2存在下笼形物熔化的H_2O-CO_2-NaCl流体包裹体的盐度有效。

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