地球科学进展 ›› 2015, Vol. 30 ›› Issue (6): 654 -667. doi: 10.11867/j.issn.1001-8166.2015.06.0654

综述与评述 上一篇    下一篇

岩浆侵入作用影响碎屑围岩储层的研究进展与展望
刘超 1, 谢庆宾 1, 王贵文 1, 崔宇 2, 张楚珺 1   
  1. 1. 中国石油大学(北京)地球科学学院 北京 102249; 2. 中石油大港油田公司勘探开发研究院 天津 300270
  • 出版日期:2015-06-25
  • 基金资助:

    国家科学自然基金项目“辉绿岩热液作用对围岩储层影响的机理研究”(编号:41272162)资助

The Influence of Igneous Intrusion to Detrital Reservoir: Advances and Outlook

Liu Chao 1, Xie Qingbin 1, Wang Guiwen 1, Cui Yu 2, Zhang Chujun 1   

  1. 1. Geosciences Department, China University of Petroleum,Beijing, Beijing 102249,China; 2. Researching Institute of Petroleum Exploration and Development of Dagang Oilfield, CNPC, Tianjin 300270, China
  • Online:2015-06-25 Published:2015-06-25

勘探实践表明,受岩浆侵入改造的变质泥岩能够成为良好的油气储层,同时岩浆侵入引发热对流和提供热液而影响砂岩围岩储层,因此探讨岩浆侵入对碎屑围岩的影响作用及其机理对于扩大油气勘探领域和储层评价具有重要意义。紧密围绕这一知识体系,概述了岩浆侵入影响沉积围岩的过程、侵入活动与油气储层的关系,归纳了国内外的主要研究进展,并从储层储集性能的角度,结合自身研究,总结了岩浆侵入作用对碎屑围岩储层的影响作用,主要表现为:①挤压变形作用。包括围岩宏观上发生塑性变形或脆性破裂、微观上碎屑颗粒脆性破裂和压溶作用。②热传递及热液变质作用。包括引发热对流使砂岩围岩改造、热烘烤引发泥岩热变质以及形成明显的变质构造。③直接或间接为成岩作用提供物质来源,产生溶蚀或沉淀。这些因素对储层储集性能具有双重作用。在此基础上,尝试探讨了今后的主要研究方向:热对流机理研究、侵入作用的影响范围,研究和建立不同侵入特征对围岩储层影响的机理并建立相应的模式。

The practice of oil and gas exploration shows that the metamorphic mudstones (slates and hornfels) can be profitable hydrocarbon plays when their petrophysical properties are transformed by igneous intrusion. Meanwhile, igneous intrusions surely effect sandstone country rocks by providing hydrothermal fluids and causing hydrothermal convection. It has great significance to explore the influencing factors and mechanism of intrusive body to country rocks as it is an important aspect to take account in reservoir evaluation and expanding hydrocarbon exploring regime. From this perspective, this paper generally summarizes the intruding and influencing process, the relationship between intrusive activities and hydrocarbon reservoirs, and the major study progresses. From standpoint of reservoir properties (porosity and permeability) and author’s case studies, the influencing factors of intrusion to country rocks are concluded as following aspects. They are: ①pressing deformation mechanism. This mechanism includes plastic deformation or brittle fracturing in macroscopy, detrital grain fracturing and pressure dissolution in microscopy. ②heat transferring and hydrothermal metamorphism. Sandstone country rocks are transformed by hydrothermal convection. Thermal metamorphism of mudstone occurs due to heat baking. Metamorphic geological structures are formed. ③intruding activities provide material sources for diagenesis directly and indirectly, causing dissolution or precipitation. These influencing factors have double effects on country rocks. On the basis of thorough discussion and conclusion above, further studies are proposed in this paper. Hydrothermal convection mechanism study, determining intrusion's influencing range, studying influencing mechanism of different intruding conditions and intrusion characteristics and establishing corresponding models are the main focus for further exploration of influencing mechanisms of igneous intrusions.

中图分类号: 

[1] Einsele G, Gieskes J M, Curray J, et al. Intrusion of basaltic sills into highly porous sediments, and resulting hydrothermal activity[J].Nature, 1980,283:442-445.
[2] Othman R, Arouri K, Warol C R, et al. Oil generation by igneous intrusions in the northern Gunnedah Basin, Australia[J].Organic Geochemistry, 2013,32(10):1 219-1 232.
[3] Wu Changzhi, Gu Lianxing, Zhang Zunzhong, et al. Formation mechanisms of hydrocarbon reservoirs associated with volcanic and subvolcanic intrusive rocks: Examples in Mesozoic-Cenozoic basins of eastern China[J].AAPG Bulletin, 2006,90(1):137-147.
[4] Renato M, Darros de Matos. The northeast Brazilian rift system[J].Tectonics, 1992, 11(4):766-791.
[5] Tao Hongxing, Xu Yuanxiu. Hydrothermal activity and oil-gas reservoir[J].Petroleum Exploration and Development, 1995,21(6):92-98.[陶洪兴,徐元秀.热液作用与油气储层[J].石油勘探与开发,1995,21(6):92-98.]
[6] Kingston D R, Dishroon C P, Williams P A. Hydrocarbon plays and global basin classification[J]. Oil & Gas Journal, 1985, 6:265-270.
[7] Gage M S, Wing R S. Southeast Asian Basin: Types versus oil opportunities[C]//Proceedings of the Annual Convention-Indonesian Petroleum Association. 1985,9:123-147.
[8] Luo Jinglan, Sadoon Morad, Liang Zhigang, et al. Controls on the quality of Archean metamorphic and Jurassic volcanic reservoir rocks from the Xinglongtai buried hill, western depression of Liaohe Basin, China[J].AAPG Bulletin, 2005,89(10):1 319-1 346.
[9] Liu Kuiyuan, Kang Renhua, Wu Hengzhi, et al. Characteristics of distribution and reservoir forming of the intrusive oil reservoir in Well-block Luo-151[J].Petroleum Exploration and Development, 2000,27(6):16-18.[刘魁元,康仁华,武恒志,等.罗151井区侵入岩油藏储集层分布及成藏特征[J].石油勘探与开发, 2000,27(6):16-18.]
[10] Zhang Cuimei, Li Qi, Su Ming. Igneous reservoirs characteristics around well Luo 151, Jiyang Sag[J].Natural Gas Exploration and Development, 2006, 29(3):17-20.[张翠梅,李琦,苏明.济阳坳陷罗151井区火成岩储层特征[J].天然气勘探与开发, 2006, 29(3):17-20.]
[11] Zhang Xiaoli, Feng Qiao, Zha Ming, et al. The influence of volcanism on clastic reservoirs in Huimin depression[J].Acta Geglogica Sinica, 2008,82(5):655-662.[张小莉,冯乔,查明,等.惠民凹陷岩浆作用对碎屑岩储层的影响[J].岩石学报,2008,82(5):655-662.]
[12] Cao Yingchang, Jiang Zaixing, Qiu Longwei. Study on the type and origin of the reservoir space of igneous oil reservoir in Shang 741 block, Huimin depression, Shandong[J].Acta Petrologica Sinica, 1999,15(1): 129-136.[操应长,姜在兴,邱隆伟.山东惠民凹陷商741块火成岩油藏储集空间类型及形成机理探讨[J].岩石学报, 1999, 15(1): 129-136.]
[13] Feng Qiao, Tang Xiyuan. Magma activity’s influence on conditions forming oil and gas pools[J]. Geological Science and Technology Information, 1997,16(4):59-65.[冯乔,汤锡元.岩浆活动对油气藏形成条件的影响[J].地质科技情报, 1997,16(4):59-65.]
[14] Ye Shaodong, Zheng Yuancai, Lu Lixia. Analysis of reservoir condition of mudstone metamorphic zone near diabase in Gaoyou Sag[J]. Complex Hydrocarbon Reservoirs, 2010,3(1):20-22.[叶绍东,郑元财,卢黎霞.高邮凹陷辉绿岩变质带储集条件分析[J].复杂油气藏, 2010, 3(1):20-22.]
[15] Zhang Yinghong, Gu Jiayu. Hydrothermal circular flow—Significant influence on reservoir in intrusion rock-metamorphic zone[J].Special Oil and Gas Reservoirs, 2003,10(1):86-89.[张映红,顾家裕.热液环流一侵入岩——外变质带储层发育的重要影响因素[J].特种油气藏,2003,10(1):86-89.]
[16] Li Yahui. Diabase and hydrocarbon reservoir formation on the northern slope of Gayou Sag[J]. Journal of Geomechanics,2000,6(2):18-21.[李亚辉.高邮凹陷北斜坡辉绿岩与油气成藏[J].地质力学学报, 2000, 6(2): 18-21.]
[17] Mao Fengming. Determination of the forming time of diabase in the northern slopeof Gaoyou Sag and it’s relationship with oil and gas[J].Petroleum Exploration and Development, 2000,27(6):19-20.[毛凤鸣.高邮凹陷北斜坡辉绿岩形成时期的确定及其与油气关系[J].石油勘探与开发,2000, 27(6):19-20.]
[18] Dow W G. Kerogen studies and geological interpretations[J].Journal of Geochemical Exploration, 1977, 7(2): 79-99.
[19] Simoneit B R T, Brenner S, Peters K E. Thermal alteration of cretaceous black shale by basaltic intrucsions in the eastern Atlantic[J].Nature, 1978,273 (5 663): 501-504.
[20] Leif R N, Simoneit B R T. Ketones in hydrothermal petroleums and sediment extracts from Guaymas Basin, Gulf of California[J].Organic Geochemistry, 1995, 23:889-904.
[21] Luiz Fernando De Ros. Heterogeneous generation and evolution of diagenetic quartzarenites in the Silurian-Devonian Furnas Formation of the Parana Basin, southern Brazil[J].Sedimentary Geology, 1998, 116:99-128.
[22] McKinley J, Worden R H, Ruffell A H, et al. Contact diagenesis: the effect of an intrusion on reservoir quality in the Triassic Sherwood sandstone group, northern Ireland[J].Journal of Sedimentary Research, 2001, 71(3): 484-495.
[23] Summer N S, Avner Ayalon. Dike intrusion into unconsolidated sandstone and the development of quartzite contact zones[J]. Journal of Structural Geology, 1995,17(7):997-1 010.
[24] Jean-Pierre Girard, Daniel Nahon. Diagenesis of the upper Proterozoic siliciclastic sediments of the Taoudeni Basin(west Africa) and relation to diabase emplacement[J].Journal of Sedimentary Petrology, 1989, 59(2):233-248.
[25] Wang Ying, Xie Donglin, Xue Chenggang. Diabase intrusion and its influence to oil and gas reservoir—Take example from Ef3 of mid-east regiion, northern slope, Gaoyou Sag[J].Journal of Oil and Gas Technology, 2010,32(2):174-177.[王颖,谢东霖,薛成刚.辉绿岩侵入作用对油气储层的影响——以高邮凹陷北斜坡中东部地区阜三段为例[J].石油天然气学报,2010,32(2):174-177.]
[26] Jaeger J C. The temperature in the neighborhood of a cooling intrusive sheet[J]. American Journal of the Medical Sciences, 1957,225:306-318.
[27] Jaeger J C. Temperatures outside a cooling intrusive sheet[J]. AmericanJournal of the Medical Sciences, 1959, 257:44-54.
[28] Brauckmann F J, Hans Fuchtbauer. Alterations of cretaceous siltstones and sandstontes near basalt contacts(Nûgssaud Greenland)[J]. Sedimentary Geology, 1983,35(1 983):193-213.
[29] Liu Li, Peng Xiaolei, Gao Yuqiao, et al. The effect of magmatic activity on clastic rocks and its contribution to diagenesisin northeast and north China petroleum-Isostasy model for bearing basin[J].Global Geology, 2003,22(4):319-325.[刘立,彭晓蕾,高玉巧,等. 东北及华北含油气盆地岩浆活动对碎屑岩的改造与成岩作用贡献[J].世界地质,2003,22(4):319-325.]
[30] Walther J V, Orville P M. Volatile production and transport in regional metamorphism[J]. Contributions to Mineralogy and Petrology, 1982,79(3):252-257.
[31] Flowers G C, Helgeson H C. Equilibrium and mass transfer during progressive metamorphism of siliceous dolomites[J]. American Journal of Science, 1983,283(3):230-286.
[32] Qian Zheng. A conceptual model of Luo151 igneous reservoir in Jiyang depression[J]. Petroleum Exploration and Development, 1999,26(6):72-75.[钱峥.济阳坳陷罗151块火成岩油藏储集层概念模型[J].石油勘探与开发,1999,26(6):72-75.]
[33] Kang Renhua, Liu Kuiyuan, Qian Zheng. Lower Tertiary diabase construction and reservoir forming features in Luojia area[J]. Special Oil & Gas Reservoirs, 2000,7(2):8-11.[康仁华,刘魁元,钱峥.罗家地区下第三系辉绿岩建造及成藏特征[J].特种油气藏,2000,7(2):8-11.]
[34] Wu Xiaozhou. A brief introduction of the diabase and contact metamorphic rock reservoirs[J]. Petroleum Exploration and Development, 1989,3:72-75.[吴小洲.辉绿岩及其接触变质岩储层简介[J].石油勘探与开发,1989,3:72-75.]
[35] Gallagher J J, Friedman M, Handin J, et al. Experimental studies relating to microfracture in sandstone[J]. Tectonophysics, 1974, 21:203-247.
[36] Sprunt E S, Nur A. Destruction of porosity through pore pressure solution[J]. Geophysics, 1977,42:726-741.
[37] Luan F C, Paterson M S. Preparation and deformation of synthetic aggregates of quartz[J]. Geophysical Research, 1992, 97:301-320.
[38] Liu Li, Yu Junming, Sun Xiaoming, et al. Basic characteristics of thermal convection diagenesis and its significance[J].Advances in Earth Science, 2000,15(5):583-585.[刘立,于均民,孙晓明,等. 热对流成岩作用的基本特征与研究意义[J].地球科学进展,2000,15(5):583-585.]
[39] Wood J R. Reservoir diagenesis and convective fluid flow[M]//MeCdonald D A, ed. Clasic Diagenesis. AAPG, Memoir 37.1984:99-110.
[40] Knut Bjorlykke, Egeberg P K. Quartz cementation in sedimentary basins[J].AAPG Bulletin, 1993,77:1 538-1 548.
[41] Haszeldine R S, Samson I M, Cornford C. Quartz diagenesis and convective fluid movement: Beatrice Oilfield, UK North Sea[J].Clay Minerals, 1984, 19:391-402.
[42] Rabinowicz M P, Jean-Louis Dandurand, Marc Jakubowski, et al. Convection in a North Sea oil reservoir: Inferences on diagenesis and hydrocarbon migration[J].Earth and Planetary Science Letters, 1985, 74(4):387-404.
[43] Enrique Merino, Jean-Pierre Girard, May M T, et al. Diagenetic mineralogy, geochemistry, and dynamics of Mesozoic arkoses, Hartford rift basin, Connecticut, U.S.A[J].Society of Sedimentary Geology, 1997,67(1):212-224.
[44] Zeng Jianhui. Hydrothermal fluids activity and its influence on fluids-rock reaction[J]. Geosicences, 2000, 25(2): 133-142.[曾溅辉.东营凹陷热流体活动及其对水—岩相互作用的影响[J].地球科学, 2000, 25(2): 133-142.]
[45] Zhang Yinghong, Zhu Xiaomin, Wu Xiaozhou, et al. Intrusive rocks and its outer metamorphic belt’s petrofacies and reservoir model[J].Petroleum Exploration and Development, 2000, 27(2):22-26.[张映红,朱筱敏,吴小洲,等.侵入岩及其外变质带岩相与储集层模型[J].石油勘探与开发,2000,27(2):22- 26.]
[46] Xiao Shangbin, Jiang Zaixing, Cao Yingchang,et al. A Preliminary approach to the classification of oil and gas reservoirs in igneous rocks[J].Special Oil & Gas Reservoirs, 1999, 21(4): 324-327.[肖尚斌,姜在兴,操应长,等.渤海湾盆地火成岩及其相关油气藏分类[J].特种油气藏,1999, 21(4): 324-327.]
[47] Degraff J M, Atilla Aydin. Surface morphology of columnar joints and its significance to mechanics and direction of joint growth[J].Geological Society of America, 1987, 99:605-617.
[48] Barnes S J, Coats C J A, Naldrett A J. Pedogenesis of a proterozoic nickel sulphide-komatiite association: The Katiniq sill, Ungava, Quebec[J].Economic Geology, 1982,77:413-429.
[49] Huber N K, Rinehart C D. Cenozoic Volcanic Rocks of the Devils Postpile Quadrangle, Eastern Sierra Nevada, California[M]. California: US Government Printing Office, 1967.
[50] Young G M. Origin of enigmatic structures: Field and geochemical investigation of columnar joints in sandstones, island of Bute, Scotland[J].The Journal of Geology, 2008, 116(5):527-536.
[51] Adamovic J. Thermal effects of magma emplacement and the origin of columnar jointing in host sandstones[C]//Thomson K, ed. LASI II: Physical Geology of Subvolcanic Systems: Laccoliths, Sills and Dykes, 2006.
[52] Peng Xiaolei. The Influence of Magmatic Activity on the Alteration of the Sandstone in the Petroleum-bearing Basin—Taking the Songliao Basin and Outward Mesozoic Basins for Examples[D]. Jilin: Jilin University, 2006.[彭晓蕾.含油气盆地中岩浆活动对砂岩的改造——以松辽盆地及其外围中生代盆地为例[D]. 吉林:吉林大学,2006.]
[53] Heald M T, Rention J J. Experimental study of sandstone cementation[J].Journal of Sedimentary Petrology, 1966, 36(4):977-991.
[54] Xu Tongtai, Wang Xingxin, Zhang Youyu, et al. Clay Minerals in Hydrocarbon-Bearing Basins of China[M].Beijing: Petroleum Industry Press, 2003:233-236.[徐同台,王行信,张有瑜,等.中国含油气盆地粘土矿物[M].北京:石油工业出版社,2003:233-236.]
[55] Wycherley H, Fleet A, Shaw H. Some observations on the origins of large volumes of carbon dioxide accumulations in sedimentary Basins Thematic set on geofluids[J].Marine and Petroleum Geology, 1999, 16:489-494.
[56] Baker J C, Bai G P, Joe Hamilton P, et al. Continental-scale magmatic carbon dioxide seepage recorded by dawsonite in the Bowen-Gunnedah-Sydney Basin system, eastern Australia[J].Society of Sedimentary Geology, 1995, 65(3):522-530.
[57] Gao Yuqiao, Liu Li. Basic characteristics of dawsonite-bearing sandstone and its geologic significance[J].Geological Review, 2007,53(1):104-111.[高玉巧,刘立.含片钠铝石砂岩的基本特征及地质意义[J].地质论评,2007,53(1):104-111.]
[58] Du Wenhua. A secondary dawsonite[J].Scentia Geologica Sinica,1992,4:434-438.[杜韫华.一种次生的片钠铝石[J].地质科学,1992,4:434-438.]
[59] Xu Yanbin, Chen Ping, Xu Yongcheng. NAICO 3 (OH) 2 : Distribution and its relationship oil and gas in Hailar Basin[J].Oil & Gas Geology, 1994,15(4):322-327.[徐衍彬,陈平,徐永成.海拉尔盆地碳钠铝石分布与油气的关系[J].石油与天然气地质,1994,15(4):322-327.]
[60] He Jiaxiong, Chen Gang. Carbon dioxide distribution and preliminary predicting studying of Yingehai Basin[J].Petroleum Exploration and Development,1998,25(2):20-26.[何家雄,陈刚.莺歌海盆地CO 2 分布及初步预测研究[J].石油勘探与开发,1998,25(2):20-26.]
[61] Guoyi Dong, Gregg Morrison, Subhash Jaireth. Quartz textures in epithermal veins, Queensland-classification, origin, and implication[J].Economic Geology, 1995, 90:1 841-1 856.
[62] Huang Shanbing. The characteristics of dawsonite stone reservoirs of the Funing formation in Jinhu Sag and its influence on reservoir properties[J].Petroleum Exploration and Development, 1996,23(2):32-34.[黄善炳.金湖凹陷阜宁组砂岩中片钠铝石特征及对物性的影响[J]. 石油勘探与开发,1996,23(2):32-34.]
[63] JonesM C, Persichetti J M. Convective instability in packed beds with throughflow[J]. AICHE Journal, 1986, 32:1 555-1 557.
[64] Nield D A. Onset of convection in a porous layer saturated by an ideal gas[J]. International Journal of Heat and Mass Transfer, 1982, 25:1 605-1 606.
[65] Riahi D N. Non-linear convection in a porous payer with permeable boundaries[J]. International Journal of Non-linear Mechanics Cracyli, 1989,24:459-463.
[66] Knut Bjorlykke, Mo A, Palm E. Modelling of thermal convectionin sedimentary basins and its relevance to diagenetic reactions[J].Marine and Petroleum Geology, 1988,5:338-350.
[67] Knut Bjorlykke. Pore-water flow and mass transfer of solids in solution in sedimentary Basins[C]//Quantitative Diagenesis: Recent Developments and Applications to Reservoir Geology. 1994.
[68] Palm E. Rayleigh convection, mass transport, and change in porosity in layers of sandstone[J]. Journal of Geophysical Research, 1990,95:8 675-8 679.
[69] Chen Rongshu, He Sheng, Wang Qingling, et al. A preliminary discussion of magma activity on the maturation of organic matter-taking Geyucheng-Wenan area of Hebei Province as an example[J]. Petroleum Exploration & Development, 1989,16 (1): 29-37.[陈荣书,何生,王青玲,等.岩浆活动对有机质成熟作用的影响初探——以冀中葛渔城一文安地区为例[J].石油勘探与开发,1989,16 (1): 29-37.]
[70] Vaclav Suchy, Jan Safanda, Ivana Sykorova, et al. Contact metamorphism of Silurian black shales by a basalt sill: Geological evidence and thermal modeling in the Barrandian Basin[J]. Bulletin of Geosciences, 2004,79(3): 133-145.
[71] Saxby J D, Stephenson L C. Effect of igneous intrusion on oil shale at Rundle (Australia)[J]. Chemical Geology, 1987, 63:1-16.
[72] Raymond A C, Murchison D G . Development of organic maturation in the aureoles of sills and its relation to sediment compaction[J]. Fuel, 1988,67:1 599-1 608.
[73] Krynauw J R, Behr H J, Van Den Kerkhof A M. Sill emplacement in wet sediments: Fluid inclusion and cathodoluminescence studies at Crunehoga, western Drowning Maud Land, Antarctica[J]. Journal of the Geological Society, 1994,151:777-794.
[74] Wang Darui, Zhang Yinghong. Carbonate cements from outer contact metamorphic reservoirs of Bohaiwan Basin: Its formation and studying significance[J].Petroleum Exploration and Development, 2001,28(2):40-42.[王大锐,张映红.渤海湾油气区火成岩外变质储集层中碳酸盐胶结物成因研究及意义[J].石油勘探与开发, 2001,28(2):40-42.]
[75] Jing Y, Chengling Z. Diagenetic influence of chemical property and flow model of water for deep sandstone reservoirs[J].Journal of the University of Petroleum, 2000, 24:60-63.

[1] 田野,田云涛. 石墨化碳质物质拉曼光谱温度计原理与应用[J]. 地球科学进展, 2020, 35(3): 259-274.
[2] 吴春明;耿元生. 变质作用精细过程研究进展[J]. 地球科学进展, 2001, 16(6): 785-794.
[3] 唐红峰,刘丛强. 变质流体作用的元素地球化学研究[J]. 地球科学进展, 2001, 16(4): 508-513.
[4] 刘 立,于均民,孙晓明,杨庆杰. 热对流成岩作用的基本特征与研究意义[J]. 地球科学进展, 2000, 15(5): 583-585.
[5] 倪志耀,王仁民,袁建平.

元古宙蛇绿岩研究中有关问题的讨论[J]. 地球科学进展, 1999, 14(5): 468-474.

[6] 简平,杨巍然. 造山带构造年代学基本问题——论同位素体系与变质作用的关系[J]. 地球科学进展, 1998, 13(5): 452-457.
[7] 刘晓春,曲玮. 变质地质学新领域——超高压变质作用与地球动力学[J]. 地球科学进展, 1995, 10(2): 148-153.
[8] 庄育勋. 造山带变质作用PTt轨迹研究存在的问题和发展趋势[J]. 地球科学进展, 1994, 9(2): 35-40.
[9] 王官福. 前寒武纪古地磁学的研究前景[J]. 地球科学进展, 1991, 6(4): 49-50.
阅读次数
全文


摘要