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1. 新疆大学新疆中亚造山带大陆动力学与成矿预测自治区重点实验室
2. 新疆维吾尔自治区煤田地质局煤层气研究开发中心
3. 新疆亚新煤层气投资开发(集团)有限责任公司
4. 中国矿业大学资源与地球科学学院
5. 新疆维吾尔自治区煤田地质局一五六煤田地质勘探队
6. 新疆维吾尔自治区能源安全监测中心
Published:2025
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[1]侯孟芮,杨曙光,李鑫,等.中国含油气地层流体包裹体研究进展及应用[J].新疆大学学报(自然科学版中英文),2025,42(05):535-549.
[1]侯孟芮,杨曙光,李鑫,等.中国含油气地层流体包裹体研究进展及应用[J].新疆大学学报(自然科学版中英文),2025,42(05):535-549. DOI: 10.13568/j.cnki.651094.651316.2024.12.20.0001.
DOI:10.13568/j.cnki.651094.651316.2024.12.20.0001.
流体包裹体分析是油气藏机理研究的有效手段之一.本文从含油气地层流体包裹体的研究对象、研究思路、研究进展及其在油气资源成藏机理的应用四个方面进行归纳研究,梳理含油气地层流体包裹体研究现状、研究成果与现存问题.根据含油气盆地流体包裹体的相态、分布空间及物化性质,可指示油气资源生排烃时期、烃源岩成熟度、油气运移路径、成藏时间、古油藏判别,并为油气成藏机制判别提供依据.含油气盆地流体包裹体的分析研究以封闭体系、均一体系、等容体系三大假设为前提,通过恢复分析流体包裹体物化性质并结合流体包裹体形成地质动态过程,可指示油气资源成藏效应与富集程度差异性.流体包裹体均一温度不能精准限定油气成藏时间,建议结合磷灰石裂变径迹、碳酸盐岩U-Pb定年与流体包裹体定年结果,可更准确地限定油气成藏时间.深层-超深层流体包裹体均一温度不能代表捕获最小温度,建议采用激光拉曼光谱-显微测温法,结合包裹体PVTx体系,可有效限定包裹体压力参数,解决最小捕获温度问题.激光拉曼光谱无法测定液态烃包裹体有机成分含量,建议使用紫外光源或785 nm激光器的拉曼光谱仪,以减少液态烃包裹体的荧光干扰.
Fluid inclusion analysis serves as an effective tool for investigating hydrocarbon reservoir mechanisms.This study systematically reviews hydrocarbon-bearing fluid inclusions in sedimentary strata through four aspects:research targets
methodological frameworks
research advancements
and applications in hydrocarbon accumulation mechanisms.It summarizes the current research status
key achievements
and unresolved challenges in this field.The phase states
spatial distribution
and physicochemical properties of fluid inclusions in petroliferous basins constrain key parameters including hydrocarbon generation/expulsion timing
source rock maturity
migration pathways
reservoir formation timing
and paleo-reservoir identification
and provide critical constraints for hydrocarbon accumulation mechanisms.Fluid inclusion analysis in petroliferous basins is based on three fundamental assumptions:closed system
homogeneous system
and isochoric system.By reconstructing the physicochemical properties of fluid inclusions and integrating their geo dynamic formation processes
this approach effectively constrains hydrocarbon accumulation efficiency and heterogeneity in enrichment degrees.The homogenization temperatures of fluid inclusions cannot independently constrain hydrocarbon accumulation timing.Integrating apatite fission-track analysis
carbonate U-Pb dating
and fluid inclusion chronology are recommended to improve temporal calibration accuracy.Homogenization temperatures of fluid inclusions in deep to ultra-deep reservoirs fail to represent minimum entrapment temperatures.Application of laser Raman spectroscopy coupled with microthermometry
integrated with PVTx modeling
is recommended to precisely constrain pressure parameters and resolve ambiguities in minimum entrapment temperatures.Laser Raman spectroscopy cannot reliably quantify the organic composition of liquid hydrocarbon-bearing fluid inclusions.It is recommended to utilize Raman spectrometers equipped with UV excitation sources or 785 nm lasers to mitigate fluorescence interference in such inclusions.
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