柴北缘N1井储层的源控成岩演化与钙质夹层成因
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Source-rock-derived diagenetic evolution and origin of calcareous interlayer in reservoirs of well N1 in the northern Qaidam Basin
  • 作者:王爱国 ; 王震亮 ; 冷先刚 ; 吴小宁 ; 蒲磊 ; 袁旭 ; 惠涛 ; 赵健
  • 英文作者:WANG Aiguo;WANG Zhenliang;LENG Xiangang;WU Xiaoning;PU Lei;YUAN Xu;HUI Tao;ZHAO Jian;National & Local Joint Engineering Research Center for Carbon Capture and Sequestration Technology;Department of Geology in Northwest University;Changqing Oilfield Company,PetroChina;Shaanxi Yanchang Petroleum International Exploration and Development Engineering Company Limited;Qinghai Oilfield Company,CNPC;
  • 关键词:柴达木盆地 ; 成岩作用 ; 成岩演化 ; 钙质夹层
  • 英文关键词:Qaidam Basin;;diagenesis;;diagenetic evolution;;calcareous interlayers
  • 中文刊名:SYDX
  • 英文刊名:Journal of China University of Petroleum(Edition of Natural Science)
  • 机构:二氧化碳捕集与封存技术国家地方联合工程研究中心;西北大学地质学系;中国石油长庆油田分公司;陕西延长石油国际勘探开发工程有限公司;中国石油青海油田分公司;
  • 出版日期:2018-10-20
  • 出版单位:中国石油大学学报(自然科学版)
  • 年:2018
  • 期:v.42;No.229
  • 基金:国家自然科学基金项目(41402115);; 中国石油青海油田公司项目(QHKT/JL-003-004)
  • 语种:中文;
  • 页:SYDX201805001
  • 页数:13
  • CN:05
  • ISSN:37-1441/TE
  • 分类号:6-18
摘要
以柴达木盆地北缘N1井为例,通过镜下观察和地化分析,探讨埋藏成岩阶段一类钙质夹层的形成过程。结果表明:N1井储层中的钙质夹层被两期烃源岩热降解成因方解石胶结(Ca1,Ca2),含少量沥青浸染高岭石;相邻高孔渗层溶蚀作用强烈,可见残余方解石、高岭石和两期沥青(Hy1,Hy2);钙质夹层非方解石直接沉淀而成,而是在烃源岩两期生排烃控制下储层成岩演化(高岭石—Hy1—Ca1—溶蚀、高岭石—Hy2—Ca2)的结果,即早期溶蚀成因Ca1型和晚期Ca2型钙质夹层的叠加。
        Taking well N1 in the northern Qaidam Basin as an example,the formation of one type of calcareous interlayer in burial diagenetic stage was investigated using microscopic observation and geochemical analysis. The results show that the calcareous interlayers in the sandstone reservoir of well N1 are thermal degraded by the source rocks as calcite cementation(Ca1 and Ca2),which contain minor bitumen-stained kaolinite. The corrosion of adjacent porous interlayers is strong,and the residual calcite,kaolinite,as well as two episodes of bitumen(Hy1,Hy2) can be observed. The calcareous interlayers are not generated by direct precipitation of calcite,but it is a result of diagenetic evolution(Kaolinite-Hy1-Ca1-dissolution/kaoliniteHy2-Ca2) which is controlled by two epiosodes of hydrocarbon generation and expulsion in source rocks. In other words,the calcareous interlayers in well N1 results from the superposition of early-stage dissolution-generated Ca1-type and late-stage Ca2-type calcareous interlayers.
引文
[1] DUTTON S P,WHITE C D,WILLIS B J,et al. Calcite cement distribution and its effect on fluid flow in a deltaic sandstone, Frontier Formation, Wyoming[J]. AAPG Bulletin,2007,12(86):2007-2021.
    [2]严科,赵红兵.三角洲前缘储层中钙质夹层分布及成因探讨[J].西南石油大学学报(自然科学版),2014,36(1):33-38.YAN Ke,ZHAO Hongbing. A discussion on distribution pattern and genesis of the calcareous intercalation in delta front reservoir[J]. Journal of Southwest Petroleum University(Science&Technology Edition),2014,36(1):33-38.
    [3]刘丽,鲍志东,秦智,等.超低渗透储层钙质夹层分布控制因素分析:来自岩石学及成岩作用研究的微观证据[J].天然气地球科学,2016,27(6):1035-1045.LIU Li,BAO Zhidong,QIN Zhi,et al. Controlling factors of calcareous interlayer distribution in ultra-low permeability reservoirs:micro evidence from petrology and diagenesis[J]. Natural Gas Geoscience,2016,27(6):1035-1045.
    [4] DAVIS J M,ROY N D,MOZLEY P S,et al. The effect of carbonate cementation on permeability heterogeneity in fluvial aquifers:an outcrop analog study[J]. Sedimentary Geology,2006,184(3/4):267-280.
    [5]田洋,卢宗盛,权英哲,等.辽河盆地大民屯凹陷沈95区块砂岩储层中钙质夹层研究[J].岩石矿物学杂志,2009,28(2):152-160.TIAN Yang,LU Zongsheng,KWON Yongchol,et al.Calcareous interbeds in the sandstone reservoir of Shen-95Block within Damintun Sag,Liaohe Basin[J]. Acta Petrologica et Mineralogica,2009,28(2):152-160.
    [6]封从军,单启铜,时维成,等.扶余油田泉四段储层非均质性及对剩余油分布的控制[J].中国石油大学学报(自然科学版),2013,37(1):1-7.FENG Congjun,SHAN Qitong,SHI Weicheng,et al.Reservoirs heterogeneity and its control on remaining oil distribution of K1q4,Fuyu Oilfield[J]. Journal of China University of Petroleum(Edition of Natural Science),2013,37(1):1-7.
    [7]罗晓容,王忠楠,雷裕红,等.特超低渗砂岩油藏储层非均质性特征与成藏模式:以鄂尔多斯盆地西部延长组下组合为例[J].石油学报,2016,37(增1):87-98.LUO Xiaorong,WANG Zhongnan,LEI Yuhong,et al.Heterogeneity characteristics and accumulation model of ultra-low permeability sandstone reservoirs:a case study of the lower part of Yanchang Formation in the western Ordos Basin,China[J]. Acta Petrolei Sinica,2016,37(sup1):87-98.
    [8]罗晓容,张立宽,雷裕红,等.储层结构非均质性及其在深层油气成藏中的意义[J].中国石油勘探,2016,21(1):28-36.LUO Xiaorong, ZHANG Likuan, LEI Yuhong, et al.Structural heterogeneity of reservoirs and its implication on hydrocarbon accumulation in deep zones[J]. China Petroleum Exploration,2016,21(1):28-36.
    [9] LUO X,HU C,XIAO Z,et al. Effects of carrier bed heterogeneity on hydrocarbon migration[J]. Marine and Petroleum Geology,2015,68(Part A):120-131.
    [10]姚光庆,李蕙生.南阳凹陷下第三系核桃园组砂岩中碳酸盐胶结物及其成因的初步探讨[J].地球科学——中国地质大学学报,1991,16(5):549-556.YAO Guangqing,LI Huisheng. A preliminary investigation on carbonate cements and their origin in sandstones of Hetaoyuan Formation,Nanyang Depression[J]. Earth Science—Journal of China University of Geosciences,1991,16(5):549-556.
    [11]王行信,周书欣.泥岩成岩作用对砂岩储层胶结作用的影响[J].石油学报,1992,13(4):20-30.WANG Xingxin,ZHOU Shuxin. The effect of diagenesis of mudstone on the cementation of a sandstone reservoir[J]. Acta Petrolei Sinica,1992,13(4):20-30.
    [12]曾溅辉,彭继林,邱楠生,等.砂-泥岩界面碳酸盐溶解-沉淀反应及其石油地质意义[J].天然气地球科学,2006,17(6):760-764.ZENG Jianhui,PENG Jilin,QIU Nansheng,et al. Carbonate dissolution-precipitation in sandstone-shale contact and its petroleum geological meanings[J]. Natural Gas Geoscience,2006,17(6):760-764.
    [13]孙海涛,钟大康,刘洛夫,等.沾化凹陷沙河街组砂岩透镜体表面与内部碳酸盐胶结作用的差异及其成因[J].石油学报,2010,31(2):246-252.SUN Haitao,ZHONG Dakang,LIU Luofu,et al. Carbonate cementation difference and its origin between exterior and interior surfaces of lenticular sandbody in Shahejie Formation of Zhanhua Depression[J]. Acta Petrolei Sinica,2010,31(2):246-252.
    [14] DUTTON S P. Calcite cement in Permian deep-water sandstones,Delaware Basin,west Texas:origin,distribution,and effect on reservoir properties[J]. AAPG Bulletin,2008,92(6):765-787.
    [15]林承焰,侯连华,董春梅,等.辽河西部凹陷沙三段浊积岩储层中钙质夹层研究[J].沉积学报,1996,14(3):74-82.LIN Chengyan,HOU Lianhua,DONG Chunmei,et al.Study on calcareous interbeds in turbidite reservoir of Sha-3 Member of the Liaohe Western Depression[J].Aata Sedimentologica Sinica,1996,14(3):74-82.
    [16]单敬福,赵忠军,李浮萍,等.砂质碎屑储层钙质夹层形成机制及其主控因素分析[J].地质论评,2015,61(3):614-620.SHAN Jingfu, ZHAO Zhongjun, LI Fuping, et al.Mechanism and controlling factors of calcium interbeds formed in the reservoir[J]. Geological Review,2015,61(3):614-620.
    [17]韩如冰,刘强,江同文,等.钙质隔夹层特征、成因及分布:以塔里木盆地哈得油田东河砂岩为例[J].石油勘探与开发,2014,141(4):428-437.HAN Rubing,LIU Qiang,JIANG Tongwen,et al. Feature,origin and distribution of calcareous interlayers:a case of Carboniferous Donghe sandstone in Hade Oilfield,Tarim Basin,NW China[J]. Petroleum Exploration and Development,2014,141(4):428-437.
    [18] CHOWDHURY A H,NOBLE J P A. Origin,distribution and significance of carbonate cements in the Albert Formation reservoir sandstones,New Brunswick,Canada[J]. Marine and Petroleum Geology,1996,13(7):837-846.
    [19]王大锐,张映红.渤海湾油气区火成岩外变质带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.WANG Darui,ZHANG Yinghong. A study on the origin of the earbonate cements within reservoirs in the external metamorphic belt of the Bohai Bay oil-gas bearing region[J]. Petroleum Exploration and Development,2001,28(2):40-42.
    [20] ODIGI M I,AMAJOR L C. Geochemistry of carbonate cements in Cretaceous sandstones, southeast Benue Trough,Nigeria:implications for geochemical evolution of formation waters[J]. Journal of African Earth Sciences,2010,57(3):213-226.
    [21] MANSURBEG H,De ROS L F,MORAD S,et al. Meteoric-water diagenesis in late Cretaceous canyon-fill turbidite reservoirs from the Espírito Santo Basin,eastern Brazil[J]. Marine and Petroleum Geology,2012,37(1):7-26.
    [22] MANSOUR A S,RIFAI R I,SHAABAN M N. Geochemical constraint on the origin of the multi-mineralogic carbonate cements in the subsurface Middle Jurassic sandstones,Central Sinai,Egypt[J]. Journal of Geochemical Exploration,2014,143(3):163-173.
    [23]郭佳,曾溅辉,宋国奇,等.东营凹陷中央隆起带沙河街组碳酸盐胶结物发育特征及其形成机制[J].地球科学——中国地质大学学报,2014,39(5):565-576.GUO Jia,ZENG Jianhui,SONG Guoqi,et al. Characteristics and origin of carbonate cements of Shahejia Formation of Central Uplift Belt in Dongying Depression[J]. Earth Science—Journal of China University of Geosciences,2014,39(5):565-576.
    [24] WANG J,CAO Y,LIU K,et al. Pore fluid evolution,distribution and water-rock interactions of carbonate cements in red-bed sandstone reservoirs in the Dongying Depression,China[J]. Marine and Petroleum Geology,2016,72:279-294.
    [25]刘春燕,郑和荣,胡宗全,等.碎屑岩中的碳酸盐胶结特征:以鄂尔多斯盆地南部富县地区延长组长6砂体为例[J].中国科学:地球科学,2012,42(11):1681-1689.LIU Chunyan,ZHENG Herong,HU Zongquan,et al.Characteristics of carbonate cementation in clastic rocks from the Chang6 sandbody of Yanchang Formation,southern Ordos Basin[J]. Science China:Earth Sciences,2012,42(11):1681-1689.
    [26] WANAS H A. Calcite-cemented concretions in shallow marine and fluvial sandstones of the Birket Qarun Formation(Late Eocene),El-Faiyum depression,Egypt:Field,petrographic and geochemical studies:implications for formation conditions[J]. Sedimentary Geology,2008,212(1/2/3/4):40-48.
    [27] MIDDLETON H A,NELSON C S. Origin and timing of siderite and calcite concretions in late Palaeogene non-to marginal-marine facies of the Te Kuiti Group,New Zealand[J]. Sedimentary Geology,1996,103(1/2):93-115.
    [28]曾春林.柴北缘西段侏罗系构造演化及其对油气成藏的控制[D].徐州:中国矿业大学,2009.ZENG Chunlin. Jurassic tectonic evolution and its control over hydrocarbon accumulation in the North Margin of Qaidam Basin[D]. Xuzhou:China University of Mining and Technology,2009.
    [29]罗晓容,孙盈,汪立群,等.柴达木盆地北缘西段油气成藏动力学研究[J].石油勘探与开发,2013,40(2):159-170.LUO Xiaorong,SUN Ying,WANG Liqun,et al. Dynamics of hydrocarbon accumulation in the west section of the northern margin of the Qaidam Basin,NW China[J]. Petroleum Exploration and Development,2013,40(2):159-170.
    [30]张玥.柴达木盆地北缘西段第三系沉积储层砂岩的成岩作用研究[D].成都:成都理工大学,2010.ZHANG Yue. Diagenesis research on the Cenozonic reservoir sandstones in the west part of Northern Margin of Qaidam Basin[D]. Chengdu:Chengdu University of Technology,2010.
    [31]刘云田,杨少勇,胡凯,等.柴达木盆地北缘中侏罗统大煤沟组七段烃源岩有机地球化学特征及生烃潜力[J].高校地质学报,2007,13(4):703-713.LIU Yuntian,YANG Shaoyong,HU Kai,et al. Organic geochemical features of mudstone source rock from Member 7 strata of middle Jurassic age in the northern margin of Qaidam Basin and its hydrocarbon-generation potential[J]. Geological Journal of China Universities,2007,13(4):703-713.
    [32]孔红喜,赵健.柴达木盆地鄂博梁地区天然气成藏条件及富集规律研究[R].敦煌:青海油田公司勘探开发研究院,2012.
    [33] MCCREA J M. On the isotopic chemistry of carbonates and a paleotemperature scale[J]. Journal of Chemical Physics,1950,18(6):849-857.
    [34] FOUKE B W,RAKOVAN J. An integrated cathodoluminescence videocapture microsampling system[J]. Journal of Sedimentary Research,2001,71:509-513.
    [35] ZHAI D,XIAO J,ZHOU L,et al. Holocene East Asian monsoon variation inferred from species assemblage and shell chemistry of the ostracodes from Hulun Lake,Inner Mongolia[J]. Quaternary Research,2011,75(3):512-522.
    [36] FOLK R L. Petrology of sedimentary rocks[M]. Austin,Texas:Hemphill Publishing Co,1980.
    [37]尹成明,李伟民,ANDREA R,等.柴达木盆地新生代以来的气候变化研究:来自碳氧同位素的证据[J].吉林大学学报(地球科学版),2007,37(5):901-907.YIN Chengming,LI Weimin,ANDREA R,et al. Cenozoic climate changes in the Qaidam Basin,western China:evidenced from carbon and oxygen stable isotope[J]. Journal of Jilin University(Earth Science Edition),2007,37(5):901-907.
    [38]李俊武,代廷勇,李凤杰,等.柴达木盆地鄂博梁地区古近系沉积物源方向分析[J].沉积学报,2015,33(4):649-658.LI Junwu,DAI Tingyong,LI Fengjie,et al. Provenance analysis of the palaeogene in Eboliang area of Qaidam Basin[J]. Acta Sedimentologica Sinica,2015,33(4):649-658.
    [39]孙国强,吕婧文,赵明君,等.柴达木盆地鄂博梁Ⅲ号中新统成岩作用及沉积环境[J].沉积学报,2015,33(2):337-347.SUN Guoqiang,LJingwen,ZHAO Mingjun,et al. Diagenesis and sedimentary environment of miocene series in EboliangⅢarea[J]. Acta Sedimentologica Sinica,2015,33(2):337-347.
    [40]李俊武,杨承锦,李凤杰,等.柴达木盆地鄂博梁地区新近系物源分析[J].古地理学报,2015,17(2):186-197.LI Junwu,YANG Chengjin,LI Fengjie,et al. Provenance analysis of the Neogene in Eboliang area,Qaidam Basin[J]. Journal of Palaeogeography,2015,17(2):186-197.
    [41]王凤琴,王宝清.柴达木盆地北缘下侏罗统储集岩成岩作用及其对孔隙演化的影响[J].兰州大学学报(自然科学版),2006,42(5):1-6.WANG Fengqin,WANG Baoqing. Diagenesis of reservoir rocks of the lower Jurassic and its influence on porosity modification in North Qaidam Basin[J]. Journal of Lanzhou University(Natrual Sciences),2006,42(5):1-6.
    [42]陈吉,史基安,孙国强,等.鄂博梁Ⅲ号构造上、下油砂山组成岩作用及对孔隙影响[J].兰州大学学报(自然科学版),2012,48(6):1-7.CHEN Ji,SHI Ji'an,SUN Guoqiang,et al. Diagenesis of lower-upper Youshashan Formation and its impact on porosity in No.Ⅲstructure of Eboliang area[J]. Journal of Lanzhou University(Natural Sciences),2012,48(6):1-7.
    [43] XIONG D,AZMY K,BLAMEY N J F. Diagenesis and origin of calcite cement in the Flemish Pass Basin sandstone reservoir(Upper Jurassic):implications for porosity development[J]. Marine and Petroleum Geology,2016,70:93-118.
    [44] EL-GHALI M A K,EL KHORIBY E,MANSURBEG H,et al. Distribution of carbonate cements within depositional facies and sequence stratigraphic framework of shoreface and deltaic arenites,Lower Miocene,the Gulf of Suez rift,Egypt[J]. Marine and Petroleum Geology,2013,45(4):267-280.
    [45] BRIGAUD B,DURLET C,DECONINCK J,et al. The origin and timing of multiphase cementation in carbonates:impact of regional scale geodynamic events on the Middle Jurassic limestones diagenesis(Paris Basin,France)[J]. Sedimentary Geology,2009,222(3/4):161-180.
    [46] DUTTON S P,LAND L S. Meteoric burial diagenesis of Pennsylvanian arkosic sandstones,Southwestern Anadarko Basin,Texas[J]. AAPG Bulletin,1985,69:22-38.
    [47] IRWIN H,CURTIS C,COLEMAN M. Isotopic evidence for source of diagenetic carbonates formed during burial of organic-rich sediments[J]. Nature, 1977,269(5625):209-213.
    [48] SULLIVAN M D,HASZELDINE R S,FALICK A E.Linear coupling of carbon and strontium isotopes in Rotliegend Sandstone,North Sea:evidence for crossformational fluid flow[J]. Geology,1990,18:1215-1218.
    [49] ALONSO-ZARZA A M,TANNER L H. Developments in sedimentology[M]. Amsterdam:Elsevier,2010,62:1-59.
    [50]赵加凡,陈小宏,金龙.柴达木盆地第三纪盐湖沉积环境分析[J].西北大学学报(自然科学版),2005,35(3):342-346.ZHAO Jiafan,CHEN Xiaohong,JIN Long. Application of stable isotope in Tertiary saline lake of Qaidamu Basin[J]. Journal of Northwest University(Natural Science Edition),2005,35(3):342-346.
    [51]张敏,尹成明,寿建峰,等.柴达木盆地西部地区古近系及新近系碳酸盐岩沉积相[J].古地理学报,2004,6(4):391-400.ZHANG Min,YIN Chengming,SHOU Jianfeng,et al.Sedimentary facies of carbonate rocks of the Paleogene and Neogene in western Qaidam Basin[J]. Journal of Palaeogeography,2004,6(4):391-400.
    [52]金强,查明.柴达木盆地西部第三系蒸发岩与生油岩共生沉积作用研究[J].地质科学,2000,35(4):465-473.JIN Qiang, ZHA Ming. Cosedimentation of Tertiary evaporites and oil source rocks in the westren Qaidam Basin[J]. Scientia Geologica Sinica,2000,35(4):465-473.
    [53] FLEISCHER M. Data of Geochemistry[M]. Amsterdam:US Geological Survey Professional,1977,440kk:KK1-KK12.
    [54] QIU N. Tectono-thermal evolution of the Qaidam Basin,China:evidence from Roand apatite fission track data[J]. Petroleum Geoscience,2002,8(3):279-285.
    [55] CAROTHERS W W,KHARAKA Y K. Aliphatic acid anions in oil-field waters:implications for origin of natural gas[J]. AAPG Bulletin,1978,62(12):2441-2453.
    [56] DIAS R F,FREEMAN K H,LEWAN M D,et al.δ13C of low-molecular-weight organic acids generated by the hydrous pyrolysis of oil-prone source rocks[J].Geochimica et Cosmochimica Acta, 2002,66(15):2755-2769.
    [57] MEANS J L,HUBBARD N. Short-chain aliphatic acid anions in deep subsurface brines:a review of their origin,occurrence,properties,and importance and new data on their distribution and geochemical implications in the Palo Duro Basin,Texas[J]. Organic Geochemistry,1987,11(3):177-191.
    [58] SURDAM R C,CROSSEY L. Organic-inorganic interactions and sandstone diagenesis[J]. AAPG Bull,1989,73:1-23.
    [59]王琪,禚喜准,陈国俊,等.延长组砂岩中碳酸盐胶结物氧碳同位素组成特征[J].天然气工业,2007,27(10):28-32.WANG Qi,ZHUO Xizhun,CHEN Guojun,et al. Characteristics of carbon and oxygen isotopic compositions of carbonate cements in Triassic Yanchang sandstone in Ordos Basin[J]. Natural Gas Industry,2007,27(10):28-32.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700