| 琼东南盆地崖城地区流体包裹体特征和油气充注期次分析 |
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| 引用本文： | 贾元琴,胡沛青,张铭杰,张同伟,陈克娜,丛亚楠.琼东南盆地崖城地区流体包裹体特征和油气充注期次分析[J].沉积学报,2012,30(1):189-196. |
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| 作者姓名： | 贾元琴 胡沛青 张铭杰 张同伟 陈克娜 丛亚楠 |
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| 作者单位： | 1. 兰州大学资源环境学院石油天然气资源中心,兰州,730000
2. 兰州大学资源环境学院石油天然气资源中心,兰州730000／西部矿产资源与地质工程教育部重点实验室,西安710054 |
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| 基金项目： | 国家科技重大专项，国家自然科学基金项目，西部矿产资源与地质工程教育部重点实验室开放基金，兰州大学萃英教授启动项目的资助 |
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| 摘 要： | 储层流体包裹体研究是油气充注期次分析的重要手段。对琼东南盆地崖城地区下第三系崖城组和陵水组砂岩储层5口钻井岩芯样品进行包裹体镜下显微观察、荧光分析和伴生盐水包裹体均一温度测量，表明该区下第三系主要发生过两期油气充注:第一期充注油气主要发淡黄色荧光，以液态烃包裹体和气液两相烃包裹体为主，伴生盐水包裹体的均一温度主要分布在130~160℃，根据区域埋藏热演化史推断油气充注时间为晚中新世-早上新世。第二期充注油气主要发淡蓝色荧光，以气态烃包裹体、气液两相烃包裹体和气液固三相烃包裹体为主，伴生盐水溶液包裹体的均一温度范围为160~190℃，充注时间应为第四纪。
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| 关 键 词： | 流体包裹体 油气运移和充注期次 储层 琼东南盆地 |
Characteristics of Fluid Inclusions and Their Constraints on Timing of Hydrocarbon Filling in the Yacheng Area of Qiongdongnan Basin,South China |
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| JIA Yuan-qin,HU Pei-qing,ZHANG Ming-jie,ZHANG Tong-wei,CHEN Ke-na,CONG Ya-nan.Characteristics of Fluid Inclusions and Their Constraints on Timing of Hydrocarbon Filling in the Yacheng Area of Qiongdongnan Basin,South China[J].Acta Sedimentologica Sinica,2012,30(1):189-196. |
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| Authors: | JIA Yuan-qin HU Pei-qing ZHANG Ming-jie ZHANG Tong-wei CHEN Ke-na CONG Ya-nan |
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| Institution: | 1(1.Center of Oil and Natural Gas Sciences,School of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000; 2.Key Laboratory of Western Mineral Resources and Geological Engineering,Ministry of Eduation,Xi’an 710054) |
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| Abstract: | The fluid inclusion of reservoir is one of important means to reveal the time of oil and natural gas charging.In present study the time of oil and natural gas charging in Yacheng and Lingshui Formation in Yacheng area of the Qiongdongnan Basin,southern China have been investigated by the analysis of type,distribution,fluorescence and homogenization temperature of fluid inclusions in samples of 5 Wells.The results indicated that the oil and natural gas bearing hydrothermal fluids have been charged twice into the sandstone reservoirs in the Paleogene reservoir.The first charge stage was characterized by condensate-gas with buff-yellow fluorescent light,its hydrocarbon fluid inclusions are dominated by liquid hydrocarbon inclusions and gas-liquid hydrocarbon inclusions,and the homogenization temperature(Th) of coeval aqueous inclusions ranges from 130℃ to 160℃.The time of first condensate-gas charging had been estimated at late Miocene to early Pliocene based on the regional burial thermal evolution history.The second charged stage was characterized by oil and natural gas with light blue fluorescence.Their hydrocarbon fluid inclusions were dominanted by gas hydrocarbon inclusions,gas-liquid hydrocarbon inclusions and three-phase hydrocarbon inclusions,the Th of coeval aqueous inclusions showed higher range from 160℃ to 190℃ than the 1st charged stage,and the charging time was estimated as Quaternary. |
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| Keywords: | fluid inclusion times of hydrocarbon charging and migration reservoir Qiongdongnan basin |
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