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Synthetic saline-aqueous and hydrocarbon fluid inclusions trapped in calcite at temperatures and pressures relevant to hydrocarbon basins: A reconnaissance study

机译:在与油气盆地有关的温度和压力下,方解石中夹带的合成盐水和烃类流体包裹体:一项侦查研究

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摘要

We conducted reconnaissance experiments to synthesize aqueous and hydrocarbon inclusions trapped in calcite at conditions relevant to petroleum basins, and characterize the microthermometric properties of such inclusions. Fluid inclusions (FIs) were synthesized in a system of saline aqueous solution (5 or 20 wt % NaCl) coexisting with either heavy crude oil or gasoline under gas-undersaturated conditions, from 90 to 210 degrees C and 200-550 bar. The synthetic inclusions are not representative of gas-bearing systems, and methane (CH4) was not detected in any aqueous inclusions. The FIs are mainly distributed along planar healed, cracks, indicating that the inclusions formed by fracture healing in the calcite crystal. Micro thermometric measurements were conducted on coeval aqueous and hydrocarbon inclusions, and Raman spectroscopic analyses were done on aqueous inclusions, to determine the properties of FIs trapped at these conditions.
机译:我们进行了侦察实验,以在与石油盆地有关的条件下合成了方解石中捕获的含水和碳氢化合物夹杂物,并表征了这些夹杂物的微热学性质。在90-210摄氏度和200-550 bar的气体不饱和条件下,在盐水溶液(5或20 wt%NaCl)与重质原油或汽油共存的系统中合成了流体包裹体(FIs)。合成夹杂物不能代表含气系统,在任何含水夹杂物中均未检测到甲烷(CH4)。 FIs主要沿平面愈合的裂缝分布,表明在方解石晶体中由于断裂愈合而形成了夹杂物。对同时存在的含水和碳氢化合物夹杂物进行微量测温,并对含水的夹杂物进行拉曼光谱分析,以确定在这些条件下捕获的FI的性质。

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