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准噶尔盆地车排子地区下白垩统清水河组储层成岩作用及物性影响因素

万青青1,2，刘洛夫1,2，肖飞1,2，常敏1,2，吴雅君1,2，胡青1,2   

  1. 1.中国石油大学(北京)油气资源与探测国家重点实验室，北京 102249；
    2.中国石油大学(北京)盆地与油藏研究中心，北京 102249
  • 收稿日期:2015-12-08 修回日期:2016-03-04 出版日期:2016-07-10 发布日期:2016-07-10
  • 通讯作者: 刘洛夫（1958-），男，广东台山人，教授，博士，主要从事石油地质及油气地球化学研究. E-mail:liulf@cup.edu.cn.
  • 作者简介:万青青（1991-），男，湖北荆州人，硕士，主要从事储层沉积与成岩作用研究. E-mail:qingqing_wan@foxmail.com.
  • 基金资助:
    国家科技重大专项（编号：2011ZX05003-001）；国家自然科学基金（编号：41372143）联合资助.

Diagenesis and factors affecting reservoir properties of the Lower Cretaceous Qingshuihe Formation,Chepaizi area,Junggar Basin,China

Wan Qing-qing1,2，Liu Luo-fu1,2，Xiao Fei1,2，Chang Min1,2，Wu Ya-jun1,2，Hu Qing1,2   

  1. 1.State Key Laboratory of Petroleum Resources and Prospecting,China University of Petroleum(Beijing),Beijing102249,China；
    2.Basin and Reservoir Research Center,China University of Petroleum(Beijing),Beijing 102249,China
  • Received:2015-12-08 Revised:2016-03-04 Online:2016-07-10 Published:2016-07-10

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摘要： 通过岩石薄片观察、扫描电镜、X-射线衍射以及碳氧同位素分析等岩矿测试分析手段研究了准噶尔盆地车排子地区下白垩统清水河组储层的成岩作用和储层物性的影响因素。准噶尔盆地车排子地区清水河组储层主要经历了压实作用，碳酸盐、方沸石、黄铁矿和黏土矿物胶结作用，以及局部少量的长石和石英的溶蚀作用。根据胶结物的占位关系确定了研究区清水河组储层成岩演化序列，即黄铁矿胶结—方沸石胶结—碳酸盐胶结—长石和石英溶蚀。根据自生碳酸盐矿物的氧同位素值确定了研究区碳酸盐胶结发生在早成岩阶段B期。车排子地区下白垩统清水河组储层成岩相分为以下6种类型：①砾岩胶结相；②砾岩杂基充填相；③(粉)砂岩弱_中压实相；④(粉)砂岩强压实相；⑤(粉)砂岩胶结相；⑥杂(粉)砂岩杂基充填相。准噶尔盆地车排子地区清水河组储层物性直接受控于3个因素：杂基含量、压实作用以及胶结作用。杂基含量主要受控于沉积相展布，辫状分流河道和水下分流河道微相杂基含量较低，而漫滩沼泽和水下分流河道间微相杂基含量较高。压实作用主要决定于地层的埋深，研究区东南部埋深较大，故压实作用更强。胶结作用的强度不易预测，但发生时的深度小于3 800m。最后提出了车排子地区清水河组储层物性主要影响因素的综合模式。

关键词: 储层物性, 成岩相, 成岩序列, 成岩作用, 车排子地区

Abstract: Through rock thin section observation,scanning electronic microscopy(SEM),X-ray diffraction,carbon and oxygen isotope analysis and other rock & mineral analysis technologies,we studied the diagenesis and factors affecting reservoir properties of the Lower Cretaceous Qingshuihe Formation.The main diagenetic events of the reservoir are compaction,cementation of carbonate,analcime,pyrite and clay minerals and a spot of feldspar and quartz dissolution in local place.Diagenetic sequence of the Qingshuihe reservoir in the study area was identified from occupying relationship between cements,namely pyrite cementation-analcime cementation-carbonate cementation-feldspar and quartz dissolution.Carbonate cementation occurred in early diagenetic phase B in the Qingshuihe Formation according to the oxygen isotopic values of authigenic carbonate minerals.The diagenetic facies of the Lower Cretaceous Qingshuihe reservoir are:(1)conglomerate cementation facies;(2)conglomerate matrix filling facies;(3)siltstone or sandstone weak- moderate compaction facies;(4)siltstone or sandstone strong compaction facies;(5)siltstone or sandstone cementation facies;(6)graywacke or miscellaneous siltstone matrix filling facies.Properties of the Lower Cretaceous Qingshuihe reservoir are directly controlled by the following three factors:Matrix content,compaction and cementation.The content of the matrix is mainly controlled by the distribution of the sedimentary facies.Braided channel and underwater braided channel microfacies have lower matrix contents whereas back swamp and underwater distributary interchannel microfacies have higher matrix contents.The extent of compaction is mostly related to the burial depth of the formation.It is buried deeper in the southeast of the study area,so compaction is stronger there.Cementation intensity is not easy to predict,but burial depth of the strata was less than 3 800m when cementation took place.Finally,an integrated model is proposed to illustrate how theses main factors affect the properties of Qingshuihe reservoir in Chepaizi area.

Key words: Reservoir properties, Diagenetic facies, Diagenetic sequence, Diagenesis, Chepaizi area

中图分类号: 

  • TE122.2

[1]Wang Zhuozhuo,Liang Jiangping,Li Guohui,et al.Affection of diagenesis on reservoir properties and its relationship with depositional setting:A case from Upper Triassic Yanchang Formation sandstones,Laoshan[J].Natural Gas Geoscience,2008,19(2):171-177.[王卓卓,梁江平,李国会,等.成岩作用对储层物性的影响及与沉积环境的关系——以鄂尔多斯盆地劳山地区为例[J].天然气地球科学,2008,19(2):171-177.]
[2]Lian Chengbo,Zhong Jianhua,Yang Yufang,et al.Influence of Quan 4 Formation sandstone diagenesis on reservoir properties in Longxi region,Songliao Basin[J].Natural Gas Geoscience,2009,20(5):691-694.[连承波,钟建华,杨玉芳,等.松辽盆地龙西地区泉四段砂岩成岩作用对储层物性的影响[J].天然气地球科学,2009,20(5):691-694.]
[3]Wu Wenhui.Research on the Characteristics and Diagenesis of Sandstone in the Upper Paleozoic Reservoir in Ordos Basin[D].Chengdu:Chengdu University of Technology,2011:51-94.[武文慧.鄂尔多斯盆地上古生界储层砂岩特征及成岩作用研究[D].成都：成都理工大学,2011:51-94.]
[4]Wei Wei,Zhu Xiaomin,Guo Dianbin,et al.Diagenesis and its control on reservoir quality of Lower Cretaceous clastic rock reservoir in Chagan Depression of Yin-E Basin[J].Natural Gas Geoscience,2014,44(12):1933-1942.[魏巍,朱筱敏,国殿斌,等.银—额盆地查干凹陷下白垩统碎屑岩储层成岩作用及其对储层物性的影响[J].天然气地球科学,2014,44(12):1933-1942.]
[5]Peters D.Recognition of two distinctive diagenesis facies trends as aid to hydrocarbon exploration in deeply buried Jurassic Smackover carbonates of southern Alabama and southern Mississippi[J].AAPG Bulletin,1985,69(2):295-296.
[6]Grigsby J D,Langsford R P.Effects of diagenesis on enhanced resolution bulk density logs in Tertiary Gulf Coast sandstones:An example from the Lower Vicksburg Formation ,McAllen Ranch field,south Texas[J].AAPG Bulletin,1996,80(11):1801-1819.
[7]Lai Jin,Wang Guiwen,Wang Shunan,et al.Research status and advances in the diagenetic facies of clastic reservoirs[J].Advances in Earth Science,2013，28(1):39-50.[赖锦,王贵文,王书南,等.碎屑岩储层成岩相研究现状及进展[J].地球科学进展,2013,28(1):39-50.]
[8]Zou Caineng,Tao Shizhen,Zhou Hui,et al.Genesis,classification and evaluation method of diagenetic facies[J].Petroleum Exploration and Development,2008,35(5):526-540.[邹才能,陶士振,周慧,等.成岩相的形成、分类与定量评价方法[J].石油勘探与开发,2008,35(5):526-540.]
[9]Chu Meijuan,Guo Zhengquan,Qi Yalin,et al.Quantitative diagenesis and diagenetic facies analysis on Chang 8 reservoir of Yanchang Formation in Ordos Basin[J].Natural Gas Geoscience,2013,24(3):477-484.[楚美娟,郭正权,齐亚林,等.鄂尔多斯盆地延长组长8储层定量化成岩作用及成岩相分析[J].天然气地球科学,2013,24(3):477-484.]
[10]Zhang Xiangxiang,Zou Caineng,Zhu Rukai,et al.Reservoir diagenetic facies of the Upper Triassic Xujiahe Formation in the central Sichuan Basin[J].Acta Petrolei Sinica,2011,32(2):257-264.[张响响,邹才能,朱如凯,等.川中地区上三叠统须家河组储层成岩相[J].石油学报,2011,32(2):257-264.]
[11]Lai Jin,Wang Guiwen,Xin Yi,et al.Diagenetic facies analysis of tight sandstone gas reservoir of Bashijiqike Formation in Kuqa Depression[J].Natural Gas Geoscience,2014,25(7):1019-1032.[赖锦,王贵文,信毅,等.库车坳陷巴什基奇克组致密砂岩气储层成岩相分析[J].天然气地球科学,2014,25(7):1019-1032.]
[12]Wang Xiuping,Mou Chuanlong.Diagenesis and diagenetic facies of reservoir in He 8 section of Shihezi Formation in east Ⅱ part of Sulige Gasfield[J].Natural Gas Geoscience,2013,24(4):678-689.[王秀平,牟传龙.苏里格气田东二区盒8段储层成岩作用与成岩相研究[J].天然气地球科学,2013,24(4):678-689.]
[13]Zhou Lu,Fu Li,Qu Jianhua,et al.Distribution of the Cretaceous Qingshuihe Formation and the favorable exploration areas in Chepaizi area[J].Journal of Southwest Petroleum University:Science & Technology Edition,2011,33(6):170-178.[周路,付立,瞿建华,等.车排子地区清水河组分布特征及有利勘探区[J].西南石油大学学报:自然科学版,2011,33(6):170-178.]
[14]Zheng Bo,Niu Wenchao,Fu Daiguo,et al.Reserves growth and exploration benefits analysis of Chunguang Exploration area[J].Petroleum Geology and Engineering,2015,29(1):11-13.[郑波,牛文朝,付代国,等.春光探区储量增长与勘探效益分析[J].石油地质与工程,2015,29(1):11-13.]
[15]Li Pilong,Feng Jianhui,Lu Yongchao,et al.Tectonic Sedimentary and Accumulation in Junggar Basin[M].Beijing:Geological Publishing House,2010:90-170.[李丕龙,冯建辉,陆永潮,等.准噶尔盆地构造沉积与成藏[M].北京:地质出版社,2010:90-170.]
[16]Yang Yongli,Lu Yongchao,Li Xiangquan,et al.Mesozoic-cenozoic sequence framework and sandstone prediction model in Chepaizi area,western Junggar Basin[J].Earth Science:Journal of China University of Geosciences,2012,37(4):743-750.[杨永利,陆永潮,李祥权,等.准西车排子地区中新生界层序格架及砂体预测模式[J].地球科学:中国地质大学学报,2012,37(4):743-750.]
[17]Zhao Dongna,Zhu Xiaomin,Dong Yanlei,et al.Sequence stratigraphic framework of Lower Cretaceous and its main controlling factors in Chepaizi area,Junggar Basin[J].Acta Sedimentologica Sinica,2013,31(6):1070-1080.[赵东娜,朱筱敏,董艳蕾,等.准噶尔盆地车排子地区下白垩统层序地层格架及主控因素分析[J].沉积学报,2013,31(6):1070-1080.]
[18]Wu Kangjun,Liu Luofu,Xiao Fei,et al.Characteristics of the hydrocarbon pathway system and transport model of the Chepaizi and its surrounding areas in the Junggar Basin of China[J].Journal of China University of Mining & Technology,2015,44(1):86-96.[吴康军,刘洛夫,肖飞,等.准噶尔盆地车排子周缘油气输导体系特征及输导模式[J].中国矿业大学学报,2015,44(1):86-96.]
[19]Xiao Fei,Liu Luofu,Zeng Liyuan,et al.Geochemical characteristics and oil source of crude oils in the east edge of Chepaizi High,Junggar Basin[J].Journal of China University of Mining & Technology,2014,43(4):646-655.[肖飞,刘洛夫,曾丽媛,等.准噶尔盆地车排子东缘原油地球化学特征与油源分析[J].中国矿业大学学报,2014,43(4):646-655.]
[20]Xia Xianbo,Jin Jun.Characteristics of Jurassic structural geology and analysis of exploration potential in Che-Guai area of Junggar Basin,China[J].Petrleum Exploration,2003,8(4):29-33.[夏显佰,靳军.准噶尔盆地西北缘车_拐地区侏罗系构造地质特征与勘探潜力分析[J].中国石油勘探,2003,8(4):29-33.]
[21]Zhuang Xinming.Petroleum geology features and prospecting targets of Chepaizi Uplift,Junggar Basin[J].Xinjiang Geology,2009,27(1):70-74.[庄新明.准噶尔盆地车排子凸起石油地质特征及勘探方向[J].新疆地质,2009,27(1):70-74.]
[22]Folk R L.Petrology of Sedimentary Rocks[M].Austin,Texas:Hemphill Publishing Company,1974:184.
[23]Sun Yushan,Liu Xinnian,Zhang Yanqiu,et al.Analcite cementation facies and forming mechanism of high-quality secondary clastic rock reservoirs in western China[J].Journal of Palaeogeography,2014,16(4):517-526.[孙玉善,刘新年,张艳秋,等.中国西部地区方沸石胶结相与碎屑岩次生优质储集层形成机制[J].古地理学报,2014,16(4):517-526.]
[24]Fu Wanjun.Influence of clay minerals on sandstone reservoir properties[J].Journal of Palaeogeography,2000,2(3):59-68.[伏万军.黏土矿物成因及对砂岩储集性能的影响[J].古地理学报,2000,2(3):59-68.]
[25]Epstein S,Buchsbaum H A,Lowenstam H,et al.Revised carbonate-water isotopic temperature scale[J].Geological Society of America Bulletin,1953,64(11):1315-1326.
[26]Gasse F,Fontes J C,Plaziat J C,et al.Biological remains,geochemistry andstable isotopes for the reconstruction of environmental and hydrological changes in the Holocene lakes from North Sahara[J].Palaeogeogr Palaeoclimatol Palaeoecol,1987,60:1-46.
[27]Fronval T,Jensen N B,Buchardt B.Oxygen isotope disequilibrium precipitation of calcite in Lake Arres,Denmark[J].Geology,1995,23(5):463-466.
[28]Teranes J L,McKenzie J A,Lotter A F,et al.Stable isotope response to lake eutrophication:Calibration of a high resolution lacustrine sequence from Baldeggersee,Switzerland[J].Limnology & Oceanography,1999,44(2):320-333.
[29]Longstaffe F J.Stable Isotope Studies of Diagenetic Processes[M]//Short Course in Stable Isotope Geochemistry of Low Temperature fluids.Quebec City:Mineralogical Association of Canada, 1987,13:187-257.
[30]Zhu Haihua,Zhong Dakang,YaoJingli,et al.Alkaline diagenesis and its effects on reservoir porosity:A case study of Upper Triassic Chang 7 tight sandstones in Ordos Basin,NW China[J].Petroleum Exploration and Development,2005,42(1):51-59.[祝海华,钟大康,姚泾利,等.碱性环境成岩作用及对储集层孔隙的影响—以鄂尔多斯盆地长7段致密砂岩为例[J].石油勘探与开发,2005,42(1):51-59.]
[31]Dove P M.The dissolution kinetics of quartz in sodium chloride solutions at 25℃ to 300℃[J].American Journal of Science,1994,294(6):665-712.
[32]Chen Zhong,Luo Zhetan,Shen Mingdao,et al.Study of secondary pore formation on the basis of chemical behavior of minerals in alkaline-flooding agents[J].Journal of Southwest China Petroleum Institute,1996,18(2):15-19.[陈忠,罗蛰潭,沈明道,等.由储层矿物在碱性驱替剂中的化学行为到砂岩储层次生孔隙的形成[J].西南石油学院学报,1996,18(2):15-19.]
[33]Zhong Dakang,Zhu Xiaomin,Zhou Xinyuan,et al.An approach to categories and mechanisms of SiO2 dissolution in sandstone reservoirs in the Tarim Basin[J].Chinese Journal of Geology:Scientia Geologica Sinica,2007,42(2):403-414.[钟大康,朱筱敏,周新源,等.初论塔里木盆地砂岩储层中SiO2的溶蚀类型及其机理[J].地质科学,2007,42(2):403-414.]
[34]Dong Yanlei,Zhu Xiaomin,Zhao Dongna.Sedimentary system and reservoir models of the Lower Cretaceous in Chepaizi area,Junggar Basin[J].Geoscience,2015,29(1):71-79.[董艳蕾,朱筱敏,赵东娜.准噶尔盆地车排子地区下白垩统沉积体系分布及油气成藏模式[J].现代地质,2015,29(1):71-79.]
[35]Zhou Changxiao,Liu Luofu,Wu Kangjun,et al.Hydrocarbon migration in sand layers of the Cretaceous Qingshuihe Formation in Chepaizi and its surrounding areas[J].Journal of Lanzhou University:Natural Sciences,2015,51(3):327-333.[周长啸,刘洛夫,吴康军,等.车排子周缘白垩系清水河组砂体油气输导特征[J].兰州大学学报:自然科学版,2015,51(3):327-333.]
[36]Zhang Zhihuan,Liu Hongjun,Li Wei,et al.Origin and accumulation process of heavy oil in Chepaizi area of Junggar Basin[J].Journal of Earth Sciences and Environment,2014,36(2):18-32.[张枝焕,刘洪军,李伟,等.准噶尔盆地车排子地区稠油成因及成藏过程[J].地球科学与环境学报,2014,36(2):18-32.]
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