STUDIES OF ACCUMULATION STAGES OF SILURIAN GAS-BEARING RESERVOIRS IN WELL KONGQUE 1 IN THE TARIM BASIN
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摘要: 近年来,塔里木盆地东北缘烃源岩高—过成熟区油气勘探获得重要发现,已在几口井中获得工业气流或油气显示,位于孔雀河斜坡维马克—开屏构造带上的孔雀1气藏是其中一个代表性的重要气藏。通过流体包裹体实验法,探讨了孔雀1井志留系含气储层的成藏期次。实验结果表明,孔雀1气藏历史上主要有2期成藏过程:第一期为加里东晚期沉积埋藏阶段古油藏形成时期(380~365 Ma);第二期为构造抬升阶段,源于古油藏热裂解成因的天然气成藏期(325~315 Ma)。对比英南2气藏的成藏时间可以看出,孔雀1气藏形成时间较早,早先建立起的孔雀河地区晚期成藏特点不具有普遍性,不同构造带具有不同的成藏历史特征。对孔雀河地区成藏历史取得的新认识,对该地区下一步油气勘探具有重要的指导意义。Abstract: Oil and gas explorations in the northeast of Tarim Basin are quite successful recently with several commercial gas accumulations discovered in high and over-matured source region.The Kongque 1(Kq 1) Gas Field,situated in the Weimake-Kaiping Structural Belt of the Kongquehe Slope,is a representative gas accumulation.With applications of organic inclusions,accumulation stages of Silurian gas-bearing reservoirs in Well Kq 1 are determined.According to experiment results,charge history of Well Kq 1 can be divided into 2 stages.The first stage is the formation time of palaeo-petroleum reservoir in de-positional phase of late-Caledonian movement(350-365 Ma).The second stage is the gas formation time during tectonic uplifting stage(325-315 Ma).Gas is thermal cracked gas derived from palaeo-petro-leum reservoirs.Compared with accumulation time of Well Yingnan 2,formation time of Well Kq 1 is earlier.Late period accumulation characters in the Kongquehe area is not general.Different tectonic belts have different oil-and-gas accumulation histories.New cognitions about formation stages of oil-and-gas are important for further explorations in the Kongquehe area.
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Key words:
- fluid inclusion experiment /
- Well Kq 1 /
- formation stages /
- Silurian /
- the Kongquehe Slope /
- the Tarim Basin
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[1] 张水昌,赵文智,王飞宇等.塔里木盆地东部地区古生界原油裂解气成藏历史分析:以英南2气藏为例[J].天然气地球科学,2004,15(5):441～451 [2] 张克银,邵志兵,邹元荣.塔里木盆地孔雀河地区复式油气系统[J].新疆石油地质,2004,25(2):122～124 [3] 杨铭,汤达祯,邢卫新等.塔里木盆地孔雀河古斜坡成藏条件新认识[J].石油实验地质,2007,29(3):275～279 [4] 欧光习,李林强,孙玉梅.沉积盆地流体包裹体研究的理论与实践[J].矿物岩石地球化学通报,2006,25(1):1～11 [5] 卢焕掌,范宏瑞,倪培等.流体包裹体[M].北京:科学出版社,2004 [6] 李荣西,席胜利,邸领军.鄂尔多斯盆地中部断裂带方解石脉天然气包裹体研究[J].石油实验地质,2006,28(5):463～466 [7] 刘德汉.包裹体研究:盆地流体追踪的有力工具[J].地学前缘,1995,2(3～4):149～154 [8] 李素梅,庞雄奇,刘可禹等.一种快速检测油包裹体的新方法[J].石油实验地质,2006,28(4):386～390 [9] Goldstein R H.Fluid inclusions in sedimentary and diagenetic systems[J].Lithos,2001,55:159～192 [10] 高玉巧,欧光习,谭守强等.歧口凹陷西坡白水头构造沙一段下部油气成藏期次研究[J].岩石学报,2003,19(2):359～365 [11] Van den Kerkhof A M,Hein U F.Fluid inclusion petrogra-phy[J].Lithos,2001,55:27～47 [12] 周雯雯,张伙兰.珠三拗陷有机包裹体应用研究[J].岩石学报,2000,16(4):677～686 [13] 李荣西,席胜利,邸领军.用储层油气包裹体岩相学确定油气成藏期次:鄂尔多斯盆地陇东油田为例[J].石油与天然气地质,2006,27(2):194～217 [14] 郑冰,承秋泉,高仁祥.塔里木盆地东北奥陶-志留系沉积成岩作用[J].石油勘探与开发,2006,27(1):85～92 [15] 王飞宇,师玉雷,曾花森等.利用油包裹体丰度识别古油藏和限定成藏方式[J].矿物岩石地球化学通报,2006,25(1):12～18 [16] Hall D,Shentwu W,Sterner M,et al.Using fluid inclusions to explore for oil and gas[J].Hart's Petroleum Engineer International,1997,(11):29～34 [17] Oxdoby N H,Mitchell A W,Gluyas J G.The filling and emptying of the Ula oilfield:fluid inclusion constrains[A].In:Cubitt J M,England W A,eds.The geochemistry of re-servoirs[G].Geological Society Special Publication,1995,86:141～157 [18] 张水昌,王招明,王飞宇等.塔里木盆地塔东2油藏形成历史[J].石油勘探与开发,2004,31(6):25～31 [19] 张忠民,周瑾,邬兴威.东海盆地西湖凹陷中央背斜带油气运移期次及成藏[J].石油实验地质,2006,28(1):30～33 [20] 宫色,彭平安,刘东鹰.江苏地区句容凹陷油气充注史研究[J].石油实验地质,2007,29(5):500～505 -
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