鄂尔多斯盆地东部奥陶系马家沟组五段5亚段微生物碳酸盐岩发育特征及储集意义

doi:10.7623/syxb202108004

石油学报 ›› 2021, Vol. 42 ›› Issue (8): 1015-1025.DOI: 10.7623/syxb202108004

鄂尔多斯盆地东部奥陶系马家沟组五段5亚段微生物碳酸盐岩发育特征及储集意义

魏柳斌^1,2,3,4, 包洪平^3,4, 严婷^3,4, 郭玮^3,4, 周黎霞^3,4, 井向辉^3,4

1. 油气藏地质及开发工程国家重点实验室四川成都 610059;
2. 成都理工大学沉积地质研究院四川成都 610059;
3. 中国石油长庆油田公司勘探开发研究院陕西西安 710018;
4. 低渗透油气田勘探开发国家工程实验室陕西西安 710018

收稿日期:2020-02-25 修回日期:2020-12-21 出版日期:2021-08-25 发布日期:2021-08-31
通讯作者: 魏柳斌,男,1987年5月生,2009年获吉林大学学士学位,2012年获成都理工大学硕士学位,现为中国石油长庆油田公司勘探开发研究院工程师,主要从事碳酸盐岩油气地质研究。
作者简介:魏柳斌,男,1987年5月生,2009年获吉林大学学士学位,2012年获成都理工大学硕士学位,现为中国石油长庆油田公司勘探开发研究院工程师,主要从事碳酸盐岩油气地质研究。Email:weilb_cq@petrochina.com.cn
基金资助:
国家科技重大专项"鄂尔多斯盆地奥陶系—元古界成藏条件研究与区带目标评价"（2016ZX05004-006）和中国石油天然气集团公司科技重大专项"鄂尔多斯盆地碳酸盐岩新领域综合研究与区带分析"（2016E-0514）资助。

Development characteristics and significance of microbial carbonate reservoirs in the fifth submember of Member 5 of Ordovician Majiagou Formation in the eastern Ordos Basin

Wei Liubin^1,2,3,4, Bao Hongping^3,4, Yan Ting^3,4, Guo Wei^3,4, Zhou Lixia^3,4, Jing Xianghui^3,4

1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Sichuan Chengdu 610059, China;
2. Institute of Sedimentary Geology, Chengdu University of Technology, Sichuan Chengdu 610059, China;
3. Research Institute of Exploration and Development, PetroChina Changqing Oilfield Company, Shaanxi Xi'an 710018, China;
4. National Engineering Laboratory for Exploration and Development of Low Permeability Oil & Gas Fields, Shaanxi Xi'an 710018, China

Received:2020-02-25 Revised:2020-12-21 Online:2021-08-25 Published:2021-08-31

摘要/Abstract

摘要： 基于钻井岩心、铸体薄片和扫描电镜等资料，研究了鄂尔多斯盆地东部马家沟组五段5亚段底部微生物碳酸盐岩的发育、分布规律及储层特征，取得了以下几点认识：①微生物碳酸盐岩的发育时期具有明显的特殊性，膏盐岩—碳酸盐岩的岩性转换期是微生物碳酸盐岩的主要发育期；②微生物碳酸盐岩的岩石类型具有明显的地域性，明显受古地貌和海水盐度控制，自东向西，由潮间带向潮下带海水盐度逐渐降低，微生物岩的岩石类型由叠层石向凝块石转变；③微生物碳酸盐岩储层的孔隙类型具有明显的专属性，凝块石白云岩以发育晶间孔为主，叠层石白云岩以发育窗格孔为主；④凝块石白云岩受回流-渗透白云石化作用控制，呈环带状分布于中央古隆起东侧，叠层石白云岩与微生物诱导白云石化作用有关，呈层状连续分布于鄂尔多斯盆地东部米脂—神木地区。研究认为，微生物碳酸盐岩具备一定的储集性，可成为马家沟组碳酸盐岩、膏盐岩共生体系天然气勘探的重要目的层系。

关键词: 鄂尔多斯盆地, 微生物碳酸盐岩, 叠层石, 凝块石, 核形石

Abstract: Based on the data of drilling cores, casting thin sections, and scanning electron microscopy (SEM), this paper studies the development, distribution and characteristics of microbial carbonate reservoirs at the bottom of the fifth submember of Member 5 of Majiagou Formation in the eastern Ordos Basin, and gets the following understandings. (1) The development period of microbial carbonate rocks shows obviously special characteristics. The lithological transition period from gypsum rock to carbonate rock is the main development period of microbial carbonate rocks. (2) The rock types of microbial carbonate rocks have significantly regional characteristics and are obviously controlled by ancient landforms and seawater salinity. From east to west, the seawater salinity gradually decreases from the intertidal zone to the subtidal zone, and the rock types of microbolite change from stromatolite to clotted limestone. (3) The pore types of microbial carbonate reservoirs have obvious specificity. The thrombolite dolomite and the stromatolite dolomite are mainly characterized by the development of intercrystalline pores and algae framework pores, respectively. (4) Thrombolite dolomite is controlled by reflux-seepage dolomitization, and it is distributed in a ring-like shape on the east side of the central palaeohigh. The development of stromatolite dolomite with a lamellar structure is related to microbial-induced dolomitization, and it is continuously distributed in the Mizhi-Shenmu area of the eastern Ordos Basin. The research suggests that the microbial carbonate rocks have a certain degree of reservoir quality and can become an important target series of strata for gas exploration in the coexisting system of carbonate rock and gypsum rock in Majiagou Formation.

Key words: Ordos Basin, microbial carbonate rock, stromatolite, thrombolite, oncolite

中图分类号:

TE122.2

魏柳斌, 包洪平, 严婷, 郭玮, 周黎霞, 井向辉. 鄂尔多斯盆地东部奥陶系马家沟组五段5亚段微生物碳酸盐岩发育特征及储集意义[J]. 石油学报, 2021, 42(8): 1015-1025.

Wei Liubin, Bao Hongping, Yan Ting, Guo Wei, Zhou Lixia, Jing Xianghui. Development characteristics and significance of microbial carbonate reservoirs in the fifth submember of Member 5 of Ordovician Majiagou Formation in the eastern Ordos Basin[J]. Acta Petrolei Sinica, 2021, 42(8): 1015-1025.

参考文献

[1] 吴亚生, 姜红霞, 虞功亮, 等.微生物岩的概念和重庆老龙洞剖面P-T界线地层微生物岩成因[J].古地理学报, 2018, 20(5):737-775.
WU Yasheng, JIANG Hongxia, YU Gongliang, et al.Conceptions of microbialites and origin of the Permian-Triassic boundary microbialites from Laolongdong, Chongqing, China[J].Journal of Palaeogeography, 2018, 20(5):737-775.
[2] BURNE R V, MOORE L.Microbialites:organosedimentary deposits of benthic microbial communities[J].Palaios, 1987, 2(3):241-254.
[3] 罗平, 王石, 李朋威, 等.微生物碳酸盐岩油气储层研究现状与展望[J].沉积学报, 2013, 31(5):807-823.
LUO Ping, WANG Shi, LI Pengwei, et al.Review and prospectives of microbial carbonate reservoirs[J].Acta Sedimentologica Sinica, 2013, 31(5):807-823.
[4] 兰才俊, 徐哲航, 马肖琳, 等.四川盆地震旦系灯影组丘滩体发育分布及对储层的控制[J].石油学报, 2019, 40(9):1069-1084.
LAN Caijun, XU Zhehang, MA Xiaolin, et al.Development and distribution of mound-shoal complex in the Sinian Dengying Formation, Sichuan Basin and its control on reservoir[J].Acta Petrolei sinica, 2019, 40(9):1069-1084.
[5] 刘树根, 宋金民, 罗平, 等.四川盆地深层微生物碳酸盐岩储层特征及其油气勘探前景[J].成都理工大学学报:自然科学版, 2016, 43(2):129-152.
LIU Shugen, SONG Jinmin, LUO Ping, et al.Characteristics of microbial carbonate reservoir and its hydrocarbon exploring outlook in the Sichuan Basin, China[J].Journal of Chengdu University of Technology:Science & Technology Edition, 2016, 43(2):129-152.
[6] 易士威, 李明鹏, 郭绪杰, 等.塔里木盆地寒武系盐下勘探领域的重大突破方向[J].石油学报, 2019, 40(11):1281-1295.
YI Shiwei, LI Mingpeng, GUO Xujie, et al.Breakthrough direction of Cambrian pre-salt exploration fields in Tarim Basin[J].Acta Petrolei Sinica, 2019, 40(11):1281-1295.
[7] GARRETT P.Phanerozoic stromatolites:noncompetitive ecologic restriction by grazing and burrowing animals[J].Science, 1970, 169(3941):171-173.
[8] GUNDE-CIMERMAN N, BUTINAR L, SONJAK S, et al.Halotolerant and halophilic fungi from coastal environments in the Arctics[M]//GUNDE-CIMERMAN N, OREN A, PLEMENITAŠ A.Adaptation to life at high salt concentrations in Archaea, Bacteria, and Eukarya.Dordrecht, Netherlands:Springer, 2005:397-423.
[9] MONTY C.Evolving concepts on the nature and the ecological significance of stromatolites[M]//FLVGEL E.Fossil algae.Berlin Heidelberg:Springer, 1977.
[10] 胡安平, 沈安江, 杨翰轩, 等.碳酸盐岩-膏盐岩共生体系白云岩成因及储盖组合[J].石油勘探与开发, 2019, 46(5):916-928.
HU Anping, SHEN Anjiang, YANG Hanxuan, et al.Dolomite genesis and reservoir-cap rock assemblage in carbonate-evaporite paragenesis system[J].Petroleum Exploration and Development, 2019, 46(5):916-928.
[11] MANCINI E A, LLINÁS J C, PARCELL W C, et al.Upper Jurassic thrombolite reservoir play, northeastern Gulf of Mexico[J].AAPG Bulletin, 2004, 88(11):1573-1602.
[12] MANCINI E A, PARCELL W C, AHR W M.Upper Jurassic Smackover thrombolite buildups and associated nearshore facies, southwest Alabama[J].Gulf Coast Association of Geological Societies, 2006, 56:551-563.
[13] MANCINI E A, PARCELL W C, AHR W M, et al.Upper Jurassic updip stratigraphic trap and associated Smackover microbial and nearshore carbonate facies, eastern Gulf coastal plain[J].AAPG Bulletin, 2008, 92(4):417-442.
[14] 宋金民, 罗平, 杨式升, 等.塔里木盆地下寒武统微生物碳酸盐岩储集层特征[J].石油勘探与开发, 2014, 41(4):404-413.
SONG Jinmin, LUO Ping, YANG Shisheng, et al.Reservoirs of Lower Cambrian microbial carbonates, Tarim Basin, NW China[J].Petroleum Exploration and Development, 2014, 41(4):404-413.
[15] 佘敏, 胡安平, 王鑫, 等.湖湘叠层石生排烃模拟及微生物碳酸盐岩生烃潜力[J].中国石油大学学报:自然科学版, 2019, 43(1):12-22.
SHE Min, HU Anping, WANG Xin, et al.Thermocompression simulation of hydrocarbon generation and expulsion for lacustrine stromatolite and hydrocarbon generation potential of microbial carbonates[J].Journal of China University of Petroleum:Edition of Natural Science, 2019, 43(1):12-22.
[16] WARREN J K.Evaporites:sediments, resources and hydrocarbons[M].Berlin Heidelberg:Springer, 2006.
[17] SLOWAKIEWICZ M, TUCKER M E, PANCOST R D, et al.Upper Permian (Zechstein)microbialites:supratidal through deep subtidal deposition, source rock, and reservoir potential[J].AAPG Bulletin, 2013, 97(11):1921-1936.
[18] SLOWAKIEWICZ M, MIKOLAJEWSKI Z.Upper Permian main dolomite microbial carbonates as potential source rocks for hydrocarbons (W Poland)[J].Marine and Petroleum Geology, 2011, 28(8):1572-1591.
[19] SARG J F, SURIAMIN, TANAVSUU-MILKEVICIENE K, et al.Lithofacies, stable isotopic composition, and stratigraphic evolution of microbial and associated carbonates, Green River Formation (Eocene), Piceance Basin, Colorado[J].AAPG Bulletin, 2013, 97(11):1937-1966.
[20] REZENDE M F, TONIETTO S N, POPE M C.Three-dimensional pore connectivity evaluation in a Holocene and Jurassic microbialite buildup[J].AAPG Bulletin, 2013, 97(11):2085-2101.
[21] LIPINSKI C J, FRANSEEN E K, GOLDSTEIN R H.Reservoir analog model for oolite-microbialite sequences, Miocene terminal carbonate complex, Spain[J].AAPG Bulletin, 2013, 97(11):2035-2057.
[22] 周进高, 付金华, 于洲, 等.鄂尔多斯盆地海相碳酸盐岩主要储层类型及其形成机制[J].天然气工业, 2020, 40(11):20-30.
ZHOU Jinggao, FU Jinghua, YU Zhou, et al.Main types and formation mechanisms of marine carbonate reservoirs in the Ordos Basin[J].Natural Gas Industry, 2020, 40(11):20-30.
[23] 熊鹰, 姚泾利, 李凌, 等.鄂尔多斯盆地东北部奥陶系马五₁₊₂微生物碳酸盐岩沉积特征及储集意义[J].沉积学报, 2016, 34(5):963-972.
XIONG Ying, YAO Jingli, LI Ling, et al.Sedimentary characteristics and reservoir significance of microbial carbonate in Ma5₁₊₂ Member of Ordovician in northestern Ordos Basin[J].Acta Sedimentologica Sinica, 2016, 34(5):963-972.
[24] 谢康, 谭秀成, 冯敏, 等.鄂尔多斯盆地苏里格气田东区奥陶系马家沟组早成岩期岩溶及其控储效应[J].石油勘探与开发, 2020, 47(6):1159-1173.
XIE Kang, TAN Xiucheng, FENG Min, et al.Eogenetic karst and its control on reservoirs in the Ordovician Majiagou Formation, eastern Sulige gas field, Ordos Basin, NW China[J].Petroleum Exploration and Development, 2020, 47(6):1159-1173.
[25] 徐旺林, 胡素云, 李宁熙, 等.鄂尔多斯盆地奥陶系中组合内幕气源特征及勘探方向[J].石油学报, 2019, 40(8):900-913.
XU Wanglin, HU Xuyun, LI Ningxi, et al.Characteristics and exploration directions of inner gas source from the middle assemblage of Ordovician in Ordos Basin[J].Acta Petrolei Sinica, 2019, 40(8):900-913.
[26] LOGAN B W, REZAK R, GINSBURG R N.Classification and environmental significance of algal stromatolites[J].Journal of Geology, 1964, 72(1):68-83.
[27] AITKEN J D.Classification and environmental significance of cryptalgal limestones and dolomites, with illustrations from the Cambrian and Ordovician of southwestern Alberta[J].Journal of Sedimentary Research, 1967, 37(4):1163-1178.
[28] MONTY C L V.The origin and development of cryptalgal fabrics[J].Developments in Sedimentology, 1976, 20:193-249.
[29] MONTY C L V, ROUCHY J M, MAURIN A, et al.Reef-stromatolites-evaporites facies relationships from Middle Miocene examples of the gulf of Suez and the Red Sea[M]//PERYT T M.Evaporite basins.Berlin Heidelberg:Springer, 1987:133-188.
[30] PRATT B R, JAMES N P.Cryptalgal-metazoan bioherms of Early Ordovician age in the St George group, western Newfoundland[J].Sedimentology, 1982, 29(4):543-569.
[31] KENNARD J M, JAMES N P.Thrombolites and stromatolites:two distinct types of microbial structures[J].Palaios, 1986, 1(5):492-503.
[32] RIDING R.Microbial carbonates:the geological record of calcified bacterial-algal mats and biofilms[J].Sedimentology, 2000, 47(S1):179-214.
[33] WARREN J K.Evaporitic source rocks:mesohaline responses to cycles of "famine or feast" in layered brines[M]//KENDALL C G S C, ALSHARHAN A S, JARVIS I, et al.Quaternary carbonate and evaporite sedimentary facies and their ancient analogues:a tribute to Douglas James Shearman.International Association of Sedimentologists, 2012:315-392.
[34] BOSAK T, LIANG Biqing, SIM M S, et al.Morphological record of oxygenic photosynthesis in conical stromatolites[J].Proceedings of the National Academy of Sciences of the United States of America, 2009, 106(27):10939-10943.
[35] BOSAK T, BUSH J W M, FLYNN M R, et al.Formation and stability of oxygen-rich bubbles that shape photosynthetic mats[J].Geobiology, 2010, 8(1):45-55.
[36] 杨威, 魏国齐, 谢武仁, 等.川中地区龙王庙组优质储层发育的主控因素及成因机制[J].石油学报, 2020, 41(4):421-432.
YANG Wei, WEI Guoqi, XIE Wuren, et al.Main controlling factors and genetic mechanism for the development of high-quality reservoirs in Longwangmiao Formation, central Sichuan Basin[J].Acta Petrolei Sinica, 2020, 41(4):421-432.
[37] VAN LITH Y, WARTHMANN R, VASCONCELOS C, et al.Sulphate-reducing bacteria induce low-temperature Ca-dolomite and high Mg-calcite formation[J].Geobiology, 2003, 1(1):71-79.
[38] KENWARD P A, FOWLE D A, GOLDSTEIN R H, et al.Ordered low-temperature dolomite mediated by carboxyl-group density of microbial cell walls[J].AAPG Bulletin, 2013, 97(11):2113-2125.

鄂尔多斯盆地东部奥陶系马家沟组五段5亚段微生物碳酸盐岩发育特征及储集意义

Development characteristics and significance of microbial carbonate reservoirs in the fifth submember of Member 5 of Ordovician Majiagou Formation in the eastern Ordos Basin

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]	吴小力, 徐旺林, 李荣西, 李宁熙, 刘齐, 赵迪, 赵帮胜, 覃小丽, 白莹. 鄂尔多斯盆地中东部奥陶系马家沟组硫化氢成因——来自流体包裹体的证据[J]. 石油学报, 2022, 43(2): 250-261.
[2]	付锁堂, 金之钧, 付金华, 李士祥, 杨伟伟. 鄂尔多斯盆地延长组7段从致密油到页岩油认识的转变及勘探开发意义[J]. 石油学报, 2021, 42(5): 561-569.
[3]	张家强, 李士祥, 李宏伟, 周新平, 刘江艳, 郭睿良, 陈俊霖, 李树同. 鄂尔多斯盆地延长组7油层组湖盆远端重力流沉积与深水油气勘探——以城页水平井区长7₃小层为例[J]. 石油学报, 2021, 42(5): 570-587.
[4]	何登发, 包洪平, 开百泽, 魏柳斌, 许艳华, 马静辉, 成祥. 鄂尔多斯盆地及其邻区关键构造变革期次及其特征[J]. 石油学报, 2021, 42(10): 1255-1269.
[5]	陈义国, 贺永红, 王超, 葛新民, 马芳侠, 孟旺才, 葛云锦, 李晓路, 樊笑微. 鄂尔多斯盆地三叠系延长组8段非常规油藏成因与成藏模式——以盆地东南部甘泉西区为例[J]. 石油学报, 2021, 42(10): 1270-1286.
[6]	付锁堂, 付金华, 牛小兵, 李士祥, 吴志宇, 周新平, 刘江艳. 庆城油田成藏条件及勘探开发关键技术[J]. 石油学报, 2020, 41(7): 777-795.
[7]	赵靖舟, 孟选刚, 韩载华. 近源成藏——来自鄂尔多斯盆地延长组湖盆东部“边缘”延长组6段原油的地球化学证据[J]. 石油学报, 2020, 41(12): 1513-1526.
[8]	李向东, 陈海燕. 深水环境下古水流方向分析和阻塞浊流沉积的识别——以鄂尔多斯盆地桌子山地区上奥陶统拉什仲组为例[J]. 石油学报, 2020, 41(11): 1348-1365.
[9]	张磊, 乔向阳, 张亮, 吴克柳, 周伟, 白慧芳, 辛翠平, 王涛. 鄂尔多斯盆地旬邑探区延长组储层特征和开发效果[J]. 石油学报, 2020, 41(1): 88-95.
[10]	徐旺林, 胡素云, 李宁熙, 魏新善, 高建荣, 赵振宇, 李相博, 刘俊榜, 张月巧, 宋微. 鄂尔多斯盆地奥陶系中组合内幕气源特征及勘探方向[J]. 石油学报, 2019, 40(8): 900-913.
[11]	张译丹, 姜在兴, 杜克峰, 张建国, 年涛, 周学文, 罗丹婷, 王力. 鄂尔多斯盆地志丹—富县地区三叠系延长组长8油层组风暴沉积特征及意义[J]. 石油学报, 2019, 40(7): 813-822.
[12]	谭聪, 阮壮, 于炳松, 刘策, 苏玲. 鄂尔多斯盆地西缘中—晚三叠世构造-物源-古地貌体系演化——来自碎屑锆石、地球化学和岩石学的证据[J]. 石油学报, 2019, 40(6): 660-676.
[13]	樊建明, 王冲, 屈雪峰, 成良丙, 薛婷. 鄂尔多斯盆地致密油水平井注水吞吐开发实践——以延长组长7油层组为例[J]. 石油学报, 2019, 40(6): 706-715.
[14]	黄兴, 李天太, 王香增, 高辉, 倪军, 赵金省, 王琛. 致密砂岩储层可动流体分布特征及影响因素——以鄂尔多斯盆地姬塬油田延长组长8油层组为例[J]. 石油学报, 2019, 40(5): 557-567.
[15]	陈林, 陆永潮, 林卫兵, 邢凤存, 陈平, 刘璐, 胡海燕, 魏巍. 鄂尔多斯盆地西南部延长组长8油层组层序地层特征及沉积充填模式[J]. 石油学报, 2019, 40(4): 434-447.