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库车克拉2气田多期油气充注的古流体证据
引用本文:鲁雪松,刘可禹,卓勤功,赵孟军,柳少波,方世虎.库车克拉2气田多期油气充注的古流体证据[J].石油勘探与开发,2012,39(5):537-544.
作者姓名:鲁雪松  刘可禹  卓勤功  赵孟军  柳少波  方世虎
作者单位:1. 提高石油采收率国家重点实验室;2. 中国石油天然气集团公司盆地构造与油气成藏重点实验室;3. 中国石油勘探开发研究院;1. 提高石油采收率国家重点实验室;2. 中国石油天然气集团公司盆地构造与油气成藏重点实验室;3. 中国石油勘探开发研究院;4. CSIRO Earth Science and Resource Engineering;1. 提高石油采收率国家重点实验室;2. 中国石油天然气集团公司盆地构造与油气成藏重点实验室;3. 中国石油勘探开发研究院;1. 提高石油采收率国家重点实验室;2. 中国石油天然气集团公司盆地构造与油气成藏重点实验室;3. 中国石油勘探开发研究院;1. 提高石油采收率国家重点实验室;2. 中国石油天然气集团公司盆地构造与油气成藏重点实验室;3. 中国石油勘探开发研究院;1. 提高石油采收率国家重点实验室;2. 中国石油天然气集团公司盆地构造与油气成藏重点实验室;3. 中国石油勘探开发研究院
基金项目:国家科技重大专项“大型油气田及煤层气开发”(2008ZX05003)
摘    要:对库车前陆盆地克拉2气田储集层进行流体包裹体分析、荧光光谱分析、场发射扫描电镜观察、岩心显微CT扫描及油气地球化学分析,从古流体证据的角度综合研究克拉2气田多阶段油气充注过程。克拉2气田经历了中新世早中期(N1)原油充注、上新世库车组沉积期(N2)高成熟油气充注与破坏、第四系(Q1以来)高—过成熟煤成气充注的3期成藏过程。储集层中广泛分布的残余干沥青、较发育的气液两相烃包裹体、纳米孔中的残余油、现今气层和水层中较高的颗粒(抽提物)荧光指数、储集层岩石较大的热解值等均是早期原油充注的证据;残余干沥青、含沥青的3相烃包裹体、凝析油轻质正构烷烃大量损失、石蜡质和芳烃等重组分含量相对较高、金刚烷含量异常高等均是早期原油遭受气洗发生脱沥青作用的有力证据。

关 键 词:古流体  流体包裹体  充注历史  气洗作用  克拉2气田

Palaeo-fluid evidence for the multi-stage hydrocarbon charges in Kela-2 gas field, Kuqa foreland basin, Tarim Basin
Lu Xuesong,Liu Keyu,Zhuo Qingong,Zhao Mengjun,Liu Shaobo and Fang Shihu.Palaeo-fluid evidence for the multi-stage hydrocarbon charges in Kela-2 gas field, Kuqa foreland basin, Tarim Basin[J].Petroleum Exploration and Development,2012,39(5):537-544.
Authors:Lu Xuesong  Liu Keyu  Zhuo Qingong  Zhao Mengjun  Liu Shaobo and Fang Shihu
Affiliation:1. State Key Laboratory of Enhanced Oil Recovery, Beijing 100083, China; 2. Key Laboratory of Basin Structure and Hydrocarbon Accumulation, CNPC, Beijing 100083, China; 3. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China;1. State Key Laboratory of Enhanced Oil Recovery, Beijing 100083, China; 2. Key Laboratory of Basin Structure and Hydrocarbon Accumulation, CNPC, Beijing 100083, China; 3. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China; 4. CSIRO Earth Science and Resource Engineering, P.O. Box 1130, Bentley, WA 6102, Australia;1. State Key Laboratory of Enhanced Oil Recovery, Beijing 100083, China; 2. Key Laboratory of Basin Structure and Hydrocarbon Accumulation, CNPC, Beijing 100083, China; 3. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China;1. State Key Laboratory of Enhanced Oil Recovery, Beijing 100083, China; 2. Key Laboratory of Basin Structure and Hydrocarbon Accumulation, CNPC, Beijing 100083, China; 3. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China;1. State Key Laboratory of Enhanced Oil Recovery, Beijing 100083, China; 2. Key Laboratory of Basin Structure and Hydrocarbon Accumulation, CNPC, Beijing 100083, China; 3. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China;1. State Key Laboratory of Enhanced Oil Recovery, Beijing 100083, China; 2. Key Laboratory of Basin Structure and Hydrocarbon Accumulation, CNPC, Beijing 100083, China; 3. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China
Abstract:The multi-stage hydrocarbon charge process of Kela-2 gas field in the Kuqa foreland basin was studied from the perspective of palaeo-fluid evidence by the analyses of fluid inclusions, fluorescence spectroscopy, FE-SEM (field emission scanning electron microscopy) observation, core micro-CT scanning, and hydrocarbon geochemistry. The result shows that the Kela-2 gas field has experienced three periods of hydrocarbon charge process, that is charged with oil at the early-middle period of the Miocence (N1), secondly charged with high matured oil & gas at the sedimentary period of the Pliocence Kuqa Formation (N2) and then destroyed by intense tectonic compression, and thirdly charged with high-over matured coal-derived gas since the Quaternary. The widely distributed residual dry bitumen, the occurrence of gas-liquid two-phase hydrocarbon inclusions, the residual oils observed in the nanopores, the higher QGF and QGF-E index, and the higher S1, S2 values of rock pyrolysis detected in both current gas zone and water zone, are the evidence of early oil charges. The residual dry bitumen, the occurrence of gas-oil-solid (bitumen) three-phase hydrocarbon inclusions, the loss of light n-alkanes and the relatively high content of aromatic hydrocarbons in the condense oil, and the abnormally high content of diamondoid hydrocarbons, are the strong evidence of gas flushing and deasphalting.
Keywords:palaeo fluid  fluid inclusions  charge history  gas flushing  Kela-2 gas field
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