油系统识别背景下矿物中流体包裹体的重要和有用事实

Q4 Earth and Planetary Sciences
K. Jarmołowicz-Szulc
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引用次数: 0

摘要

所采取的分析步骤已确定包裹体中包裹的流体为盐水和/或碳氢化合物(基于荧光能力)。此外,它们还测量了包裹体的均质温度(例如,油的值为正,甲烷的值为负,纯的或有添加剂的),以及水包裹体的共晶温度和融冰温度的测定。加热模式下的测温研究通常会导致矿物结晶温度的测定,因为人们假设原生水包裹体的均质温度代表矿物沉淀过程中流体捕获的最低温度。补充分析,如拉曼光谱分析和有机质研究,可以对碳氢化合物系统背景下的结果进行更丰富、更清晰和有意义的解释,这在一些例子中得到了证明。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ważne i użyteczne fakty dotyczące inkluzji fluidalnych w minerałach w kontekście rozpoznawania systemów naftowych
The undertaken analytical steps have led to determination of the fluids trapped in inclusions as brine and/or hydrocarbons (based on fluorescence abilities). Furthermore, they have resulted in the measurement of the homogenization temperatures of inclusions (values positive for, e.g., oil, negative for methane, pure or with admixtures), and determinations of the eutectic and ice-melting temperatures of the aqueous inclusions. Thermometric studies in the heating mode generally lead to determination of temperatures of mineral crystallization since it has been assumed that the homogenization temperature of the primary aqueous inclusions represents a minimum temperature of fluid trapping during mineral precipitation. Complementary analyses, as the Raman spectrum analysis and studies on the organic matter, lead to the interpretation of the results richer, clearer and meaningful for the hydrocarbon systems context, what has been proved on some examples.
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来源期刊
Przeglad Geologiczny
Przeglad Geologiczny Earth and Planetary Sciences-Geology
CiteScore
0.70
自引率
0.00%
发文量
24
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