松辽盆地北部深层火山岩气藏的充注：来自流体包裹体的证据

doi:10.7623/syxb201106006

石油学报 ›› 2011, Vol. 32 ›› Issue (6): 968-975.DOI: 10.7623/syxb201106006

松辽盆地北部深层火山岩气藏的充注：来自流体包裹体的证据

肖骏 1,2 陈汉林 1 杨树锋 1 章凤奇 1 林秀斌 1 余星 3 庞彦明 4 舒萍 4

1浙江大学地球科学系浙江杭州 310027； 2中国地质大学期刊社湖北武汉 430074； 3国家海洋局第二海洋研究所浙江杭州 310012； 4大庆油田有限责任公司勘探开发研究院黑龙江大庆 163712

收稿日期:2011-05-07 修回日期:2011-08-26 出版日期:2011-11-25 发布日期:2012-01-17
通讯作者: 肖骏
作者简介:肖骏，女，1983年2月生，2011年获浙江大学理学博士学位，现为中国地质大学（武汉）期刊社编辑。
基金资助:
中国博士后科学基金面上项目（20070421162）资助。

Gas charging of deep volcanic reservoirs in the northern Songliao Basin：Evidence from fluid inclusions

XIAO Jun 1,2 CHEN Hanlin 1 YANG Shufeng 1 ZHANG Fengqi 1 LIN Xiubin 1 YU Xing 3 PANG Yanming 4 SHU Ping 4

Received:2011-05-07 Revised:2011-08-26 Online:2011-11-25 Published:2012-01-17

摘要/Abstract

摘要：

厘清松辽盆地北部徐家围子断陷营城组火山岩气藏天然气的来源和充注特征对天然气的勘探开发具有重要意义。系统研究了营城组储层中次生流体包裹体的成分和均一温度，旨在揭示天然气气藏的来源和充注特征。研究结果表明该储层中发育了富CH₄和富CO₂两类流体包裹体。富CH₄流体包裹体均一温度出现频率最高的区间包括：160～163℃、185.2～225℃和233～243.4℃，说明存在3期含烃流体；富CO₂流体包裹体均一温度为235.2～269.1℃，为一期充注。均一温度高于烃源岩沙河子组地层的最高埋深温度（230℃）的富CO₂流体包裹体和高温富CH₄流体包裹体内的天然气可能来源于深部。流体包裹体主要成分和气藏天然气主要成分对比表明，本区天然气充注存在3种充注方式：①一期天然气充注形成；②多期混合充注形成；③前期充注被后期天然气充注取代形成。

关键词: 松辽盆地, 流体包裹体, 火山岩气藏, 充注方式, 幔源成因

Abstract:

Gas sources and charging models of volcanic reservoirs are of significance in gas exploration and development, the present paper examined CH₄- and CO₂-rich fluid inclusions discovered in the Yingcheng Formation of the Xujiaweizi fault depression, northern Songliao Basin to delineate source and charging characteristics of gas reservoirs. The result indicates that homogenization temperatures of CH₄-rich fluid inclusions in various samples range from 160℃ to 243.4℃ with three most frequent intervals between 160～163℃, 185.2～225℃ and 233～243.4℃, suggesting three episodes of hydrocarbon fluid charging, while those of CO₂-rich fluid inclusions vary from 235.2℃ to 269.1℃, indicating only one episode of CO₂-rich fluid charging. Therefore, CH₄- and CO₂-rich fluid inclusions that have homogenization temperatures higher than 230℃, the highest burial temperature of Shahezi Formation source rocks, is most likely derived from deeper sources. The comparison of main components between fluid inclusions and natural gases in reservoirs indicated that three charging modes might occur in this area: (1) single episode gas charging; (2) multi-episode gas charging; and (3) replacement gas charging of the former by the latter.

Key words: Songliao Basin, fluid inclusion, volcanic gas reservoir, charging mode, mantle origin

肖骏陈汉林杨树锋章凤奇林秀斌余星庞彦明舒萍. 松辽盆地北部深层火山岩气藏的充注：来自流体包裹体的证据[J]. 石油学报, 2011, 32(6): 968-975.

XIAO Jun CHEN Hanlin YANG Shufeng ZHANG Fengqi LIN Xiubin YU Xing. Gas charging of deep volcanic reservoirs in the northern Songliao Basin：Evidence from fluid inclusions[J]. Editorial office of ACTA PETROLEI SINICA, 2011, 32(6): 968-975.

参考文献

[1]邵奎政，梁晓东.徐家围子地区天然气成藏期次及其模式[J].大庆石油地质与开发,2002,21(6):4-5.

Shao Kuizheng,Liang Xiaodong.Gas accumulation period and models in Xujiaweizi region[J].Petroleum Geology ＆ Oilfield Development in Daqing,2002,21(6):4-5.

[2]付广，吕延防，孟庆芬.松辽盆地北部深层火山岩气藏形成时期及成藏模式研究[J].中国海上油气（地质）,2003,17(4):236-239.

Fu Guang,Lü Yanfang,Meng Qingfen.A study on formation periods and accumulation models of the deep volcanic gas pools in the northern Songliao Basin[J].China Offshore Oil and Gas (Geology),2003,17(4):236-239.

[3]陶士振，刘德良，杨晓勇，等.无机成因天然气藏形成条件分析[J].天然气地球科学,2000,12(1):10-18.

Tao Shizhen,Liu Deliang,Yang Xiaoyong,et al.Analysis of forming conditions of inorganic gas pool[J].Natural Gas Geoscience, 2000,12(1):10-18.

[4]王先彬，郭占谦，妥进才，等.中国松辽盆地商业天然气的非生物成因烷烃气体[J].中国科学D辑：地球科学,2009,39(5):602-614.

Wang Xianbin,Guo Zhanqian,Tuo Jincai,et al.Abiogenic hydrocarbons in commercial gases from the Songliao Basin,China[J].Science in China Series D:Earth Sciences,2009,52(2):213-226.

[5]魏志平，张景廉，方乐华，等.松辽盆地天然气成因探讨[J].新疆石油地质,2009,30(7):537-542.

Wei Zhiping,Zhang Jinglian,Fang Lehua,et al.Controversy of the Origins of Natural Gas in Songliao Basin[J].Xinjiang Petroleum Geology,2009,30(7):537-542.

[6]周荔青，金之钧.松辽盆地无机成因气藏形成分布特征及勘探方向[J].石油实验地质,2009,31(1):12-18.

Zhou Liqinq,Jin Zhijun.Formation and distribution features of the abiogenic gas pools and their exploration strategies in the Songliao Basin[J].Petroleum Geology ＆ Experiment,2009,31(1):12-18.

[7]杨春，刘全有，周庆华，等.松辽盆地庆深气田天然气成因类型鉴别[J].地球科学(中国地质大学学报),2009,34(5):792-798.

Yang Chun,Liu Quanyou,Zhou Qinghua,et al.Genetic identification of natural gases in Qingshen gas field,Songliao Basin[J].Earth Science-Journal of China University of Geosciences,2009,34(5):792-798.

[8]张居和，方伟，李景坤，等.松辽盆地徐家围子断陷深层天然气成因类型及各种成因气贡献[J].地质学报,2009,83(4):579-589.

Zhang Juhe,Fang Wei,Li Jingkun,et al.Deep gases and their genetic types of the Xujiaweizi fault depression zone,Songliao Basin and their contribution[J].Acta Geologica Sinica,2009,83(4):579-589.

[9]李景坤,方伟,曾花森,等.徐家围子断陷烷烃气碳同位素反序机制[J].石油学报,2011,32(1):54-61.

Li Jingkun,Fang Wei,Zeng Huasen,et al.Possible origins for inverse stable carbon isotopes of gaseous alkanes from the Xujiaweizi fault depression[J].Acta Petrolei Sinica,2011,32(1):54-61.

[10]杨春，刘全有，米敬奎，等.松辽盆地大庆长垣伴生气中二氧化碳成因讨论[J].天然气地球科学,2008,19(2):244-249.

Yang Chun,Liu Quanyou,Mi Jingkui,et al.Discussion about the CO₂ origin in associated gas from Daqing Placanticline,Songliao Basin[J].Natural Gas Geoscience,2008,19(2):244-249.

[11]鲁雪松，宋岩，柳少波，等.松辽盆地幔源CO₂分布规律与运聚成藏机制[J].石油学报,2009(05):661-666.

Lu Xuesong,Song Yan,Liu Shaobo,et al.Distribution and migration-accumulation mechanism of mantle-derived CO₂ in Songliao Basin[J].Acta Petrolei Sinica,2009,30(5):661-666.

[12]杨映涛，陈恭洋，王连桥，等.松辽盆地深层CO₂气成藏主控因素分析[J].石油天然气学报,2009,31(4):54-57.

Yang Yingtao,Chen Gongyang,Wang Lianqiao,et al.Study of main control factors of deep CO₂ gas accumulation in Songliao Basin[J].Institute of Petroleum Exploration and Development,2009,31(4):54-57.

[13]冯子辉，任延广，王成，等.松辽盆地深层火山岩储层包裹体及天然气成藏期研究[J].天然气地球科学,2003,14(6):436-442.

Feng Zihui,Ren Yanguang,Wang Cheng,et al.Study on inclusion of deep buried igneous reservoir and forming period of gas pool in Songliao Basin[J].Natural Gas Geoscience,2003,14(6):436-442.

[14]Li C Q,Pang Y M,Chen H L,et al.Gas charging history of the Yingcheng Formation igneous reservoir in the Xujiaweizi Rift,Songliao Basin,China[J].Journal of Geochemical Exploration,2006,89:210-213.

[15]胡明，付广，吕延防，等.松辽盆地徐家围子断陷断裂活动时期及其与深层气成藏关系分析[J].地质论评,2010,56(5):710-718.

Hu Ming,Fu Guang,Lü Yanfang,et al.The fault activity period and its relationship to deep gas accumulation in the Xujiaweizi Depression,Songliao Basin[J].Geological Review,2010,56(5):710-718.

[16]章凤奇. 松辽盆地北部早白垩世火山事件与地球动力学[D]. 浙江大学,2007.

Zhang Fengqi.Early cretaceous volcanic event in the northern Songliao Basin and its geodynamics[D].Zhejiang University,2007.

[17]郭占谦，王连生，刘立，等.大庆长垣伴生气中二氧化碳的成因研究[J].天然气地球科学,2006,17(1):48-50.

Guo Zhanqian,Wang Liansheng,Liu Li,et al.The research of the origin of carbon dioxide in associated gas of Daqing Placanticline[J].Natural Gas Geoscience,2006,17(1):48-50.

[18]王先彬，郭占谦，妥进才，等.非生物成因天然气形成机制与资源前景[J].中国基础科学,2006,8(4):12-20.

Wang Xianbin,Guo Zhanqian,Tuo Jincai,et al.Formation mechanism and resources prospect of the abiogenic gas[J].China Basic Science,2006,8(4):12-20.

[19]王力，王可勇，葛文春，等.松辽盆地深层火山岩储层中的CH₄包裹体:产状特征及其地质意义[J].岩石学报,2008,24(9):2171-2178.

Wang Li,Wang Keyong,Ge Wenchun,et al.Methane fluid inclusions in deep level volcanic reservoir rocks in Songliao basin: Characteristics of occurrence and geological implications[J].Acta Petrologica Sinica,2008,24(9):2171-2178.

松辽盆地北部深层火山岩气藏的充注：来自流体包裹体的证据

Gas charging of deep volcanic reservoirs in the northern Songliao Basin：Evidence from fluid inclusions

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	罗涛, 郭小文, 舒志国, 包汉勇, 何生, 覃泽健, 肖智慧. 四川盆地焦石坝南部地区五峰组—龙马溪组裂缝脉体流体来源及形成时间[J]. 石油学报, 2021, 42(5): 611-622.
[2]	邓铭哲, 方成名, 邓棚, 张永, 朱建峰. 松辽盆地南部梨树地区走滑-逆冲构造的成因——以小宽断裂带为例[J]. 石油学报, 2020, 41(9): 1089-1099.
[3]	郭小文, 陈家旭, 袁圣强, 何生, 赵建新. 含油气盆地激光原位方解石U-Pb年龄对油气成藏年代的约束——以渤海湾盆地东营凹陷为例[J]. 石油学报, 2020, 41(3): 284-291.
[4]	孙立东, 陆加敏, 杨步增, 刘家军, 李晶, 张莹, 戴世立, 徐妍, 蔡东梅. 松辽盆地北部中央古隆起带天然气成藏条件与勘探方向[J]. 石油学报, 2020, 41(10): 1163-1173.
[5]	高凤琳, 宋岩, 梁志凯, 李卓, 原园, 张瀛涵, 陈磊, 郭望. 陆相页岩有机质孔隙发育特征及成因——以松辽盆地长岭断陷沙河子组页岩为例[J]. 石油学报, 2019, 40(9): 1030-1044.
[6]	鲁雪松, 赵孟军, 陈竹新, 李学义, 胡瀚文, 卓勤功. 准噶尔盆地南缘齐古油田油气成藏再认识及勘探启示[J]. 石油学报, 2019, 40(9): 1045-1058,1115.
[7]	田孝茹, 张元元, 卓勤功, 于志超, 郭召杰. 准噶尔盆地玛湖凹陷下二叠统风城组致密油充注特征——碱性矿物中的流体包裹体证据[J]. 石油学报, 2019, 40(6): 646-659.
[8]	郝国丽, 单玄龙, 李锋, 仝立华, 刘轶松, 王书琴, 张家强, 赵成弼. 松辽盆地西部斜坡油砂油地球化学及生物降解特征[J]. 石油学报, 2019, 40(3): 308-321.
[9]	孙立东, 印长海, 刘超, 曾花森, 张莹, 徐妍, 蔡东梅. 松辽盆地营城组优质烃源岩地质特征及勘探意义[J]. 石油学报, 2019, 40(10): 1172-1179.
[10]	刘建良, 刘可禹, 姜振学, 邢金艳. 库车前陆盆地玉东地区白垩系油气成藏过程[J]. 石油学报, 2018, 39(6): 620-630.
[11]	李文, 何生, 张柏桥, 何治亮, 陈曼霏, 张殿伟, 李天义, 高键. 焦石坝背斜西缘龙马溪组页岩复合脉体中流体包裹体的古温度及古压力特征[J]. 石油学报, 2018, 39(4): 402-415.
[12]	庄新兵, 顾忆, 邵志兵, 尤东华, 丁勇, 万旸璐. 塔里木盆地地温场对油气成藏过程的控制作用——以古城墟隆起为例[J]. 石油学报, 2017, 38(5): 502-511.
[13]	张敏, 欧光习, 张枝焕, 黎琼, 宫晓峰. 柴达木盆地东部石炭系页岩气储层流体地球化学特征[J]. 石油学报, 2017, 38(11): 1244-1252.
[14]	王震亮, 魏丽, 王香增, 王念喜, 范昌育, 李彦婧, 赵雪娇, 赵晓东, 任来义, 曹红霞. 鄂尔多斯盆地延安地区下古生界天然气成藏过程和机理[J]. 石油学报, 2016, 37(S1): 99-110.
[15]	冯明友, 强子同, 沈平, 张健, 陶艳忠, 夏茂龙. 四川盆地高石梯-磨溪地区震旦系灯影组热液白云岩证据[J]. 石油学报, 2016, 37(5): 587-598.