岩性油气藏 ›› 2023, Vol. 35 ›› Issue (5): 37–48.doi: 10.12108/yxyqc.20230504

• 地质勘探 • 上一篇    下一篇

鄂尔多斯盆地苏里格地区奥陶系马家沟组马五5亚段沉积特征

杜江民1,2, 崔子豪1,2, 贾志伟3, 张毅3, 聂万才4,5, 龙鹏宇1,2, 刘泊远1,2   

  1. 1. 河北地质大学 河北省战略性关键矿产资源重点实验室, 石家庄 050031;
    2. 河北地质大学 地球科学学院, 石家庄 050031;
    3. 中国石油西南油气田公司, 成都 610051;
    4. 西南石油大学 地球科学与技术学院, 成都 610500;
    5. 中国石油长庆油田分公司 天然气评价项目部, 西安 710018
  • 收稿日期:2022-09-23 修回日期:2022-11-27 出版日期:2023-09-01 发布日期:2023-09-28
  • 第一作者:杜江民（1984—），男，博士，副教授，主要从事石油地质和沉积学方面的研究工作。地址：（050031）河北省石家庄市槐安东路136号河北地质大学教务处。Email：jiangmindu@163.com。
  • 基金资助:
    河北省高等学校科学技术研究重点项目 “海相碳酸盐岩储层白云岩成因机理研究”（编号： ZD2022057） 资助。

Sedimentary characteristics of Ma 55 sub-member of Ordovician Majiagou Formation in Sulige area，Ordos Basin

DU Jiangmin1,2, CUI Zihao1,2, JIA Zhiwei3, ZHANG Yi3, NIE Wancai4,5, LONG Pengyu1,2, LIU Boyuan1,2   

  1. 1. Hebei Key Laboratory of Strategic Critical Mineral Resources, Hebei GEO University, Shijiazhuang 050031, China;
    2. College of Earth Sciences, Hebei GEO University, Shijiazhuang 050031, China;
    3. PetroChina Southwest Oil & Gas Field Company, Chengdu 610051, China;
    4. School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China;
    5. Department of Natural Gas Evaluation Project, PetroChina Changqing Oilfield Company, Xi'an 710018, China
  • Received:2022-09-23 Revised:2022-11-27 Online:2023-09-01 Published:2023-09-28

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摘要： 鄂尔多斯盆地苏里格地区奥陶系马家沟组马五5亚段勘探潜力巨大。通过岩心观察、薄片鉴定、扫描电镜分析和地球化学测试，结合地球物理技术，对苏里格地区奥陶系马家沟组马五5亚段沉积特征进行了系统研究，探讨了其油气地质意义。研究结果表明： ①苏里格地区奥陶系马家沟组马五5亚段属于整体海侵、晚期海退沉积背景下的向东倾斜的碳酸盐岩台地相，发育开阔台地和局限台地等亚相，可根据成分细分为云坪、灰坪和台内滩、云灰坪、灰云坪等微相。②研究区平面上沉积环境呈典型条带状展布，西部地区沉积水体盐度偏高，具有局限台地特征；东部地区沉积水体盐度偏低，具有开阔台地特征。③研究区的局限台地与开阔台地内部的低洼区域，高密度富Mg海水汇聚，为白云岩发育的有利区。④局限/开阔云坪相、台内滩和含膏云坪微相主要发育各种白云岩储层，连片发育白云岩的西、北部地区是潜在的油气勘探接替领域。

关键词: 开阔台地, 局限台地, 白云岩储层, 马五5亚段, 马家沟组, 奥陶系, 苏里格地区, 鄂尔多斯盆地

Abstract: The exploration potential of Ma 55 sub-member of Ordovician Majiagou Formation in Sulige area of Ordos Basin is huge. Through core observation，thin section identification，scanning electron microscope and geochemical testing，combined with geophysical technologies，the sedimentary characteristics of Ma 55 sub-member of Ordovician Majiagou Formation in Sulige area were studied，and its petroleum geological significance was discussed. The results show that： （1）The Ma 55 sub-member of Ordovician Majiagou Formation in Sulige area belongs to carbonate platform facies which inclines to the east under the background of overall transgression and late regressions. Open platform and restricted platform subfacies are developed，which can be subdivided into dolomite flat，carbonate flat，and intraplatform shoal，dolomite-carbonate flat and carbonate-dolomite flat according to the composition.（2）In the plane，the sedimentary environment is typical banded distribution，the salinity of the sedimentary water in the western region is relatively high，with restricted platform characteristics，while the salinity of the sedimentary water in the eastern region is low and has the characteristics of open platform.（3）The low-lying areas within the restricted platform and the open platform in the study area，where high-density and Mg-rich seawater converges，are favorable areas for dolomite development.（4）The restricted/open dolomite flat，intraplatform shoal and gypsum-bearing dolomite flat microfacies mainly develop various kinds of dolomite reservoirs. The western and northern areas with contiguous dolomites are potential replacement areas for oil and gas exploration.

Key words: open platform, restricted platform, dolomite reservoir, Ma55 sub-member, Majiagou Formation, Ordovician, Sulige area, Ordos Basin

中图分类号: 

  • TE121.3
[1] 邓虎成,周文,郭睿,等.伊拉克艾哈代布油田中—下白垩统碳酸盐岩储层孔隙结构及控制因素[J].岩石学报, 2014, 30(3):801-812. DENG Hucheng, ZHOU Wen, GUO Rui, et al. Pore structure characteristics and control factors of carbonate reservoirs:The Middle-Lower Cretaceous formation, AI Hardy cloth Oilfield, Iraq[J]. Acta Petrologica Sinica, 2014, 30(3):801-812.
[2] 沈安江,赵文智,胡安平,等.海相碳酸盐岩储集层发育主控因素[J].石油勘探与开发, 2015, 42(5):545-554. SHEN Anjiang, ZHAO Wenzhi, HU Anping, et al. Major factors controlling the development of marine carbonate reservoirs[J]. Petroleum Exploration and Development, 2015, 42(5):545-554.
[3] 付金华,魏新善,任军峰,等.鄂尔多斯盆地天然气勘探形势与发展前景[J].石油学报, 2006, 27(6):1-13. FU Jinhua, WEI Xinshan, REN Junfeng, et al. Gas exploration and developing prospect in Ordos Basin[J]. Acta Petrolei Sinica, 2006, 27(6):1-13.
[4] 杨华,包洪平.鄂尔多斯盆地奥陶系中组合成藏特征及勘探启示[J].天然气工业, 2011, 31(12):11-20. YANG Hua, BAO Hongping. Characteristics of hydrocarbon accumulation in the Middle Ordovician assemblages and their significance for gas exploration in the Ordos Basin[J]. Natural Gas Industry, 2011, 31(12):11-20.
[5] 朱广社,赵俊兴,邵晓岩,等.苏里格东部马五5储层特征及成藏控制因素[J].西南石油大学学报(自然科学版), 2014, 36(3):45-53. ZHU Guangshe, ZHAO Junxing, SHAO Xiaoyan, et al. Reservoir characteristics and controlling factors of M55 sub-member of Majiagou Formation in the east of Sulige area[J]. Journal of Southwest Petroleum University (Science & Technology Edition), 2014, 36(3):45-53.
[6] 侯方浩,方少仙,董兆雄,等.鄂尔多斯盆地中奥陶统马家沟组沉积环境与岩相发育特征[J].沉积学报, 2003, 21(1):106-112. HOU Fanghao, FANG Shaoxian, DONG Zhaoxiong, et al. The developmental characters of sedimentary environments and lithofacies of Middle Ordovician Majiagou Formation in Ordos Basin[J]. Acta Sedimentologica Sinica, 2003, 21(1):106-112.
[7] 董兆雄,姚泾利,孙六一,等.重新认识鄂尔多斯南部早奥陶世马家沟期碳酸盐台地沉积模式[J].中国地质, 2010, 37(5):1327-1335. DONG Zhaoxiong, YAO Jingli, SUN Liuyi, et al. The carbonate platform sedimentary model of southern Ordos Basin[J]. Geology in China, 2010, 37(5):1327-1335.
[8] 王琳霖,浮昀,方诗杰.鄂尔多斯盆地东缘马家沟组元素地球化学特征及古沉积环境[J].石油实验地质, 2018, 40(4):519-525. WANG Linlin, FU Yun, FANG Shijie. Elemental geochemical characteristics and geological significance of Majiagou Formation, eastern Ordos Basin[J]. Petroleum Geology & Experiment, 2018, 40(4):519-525.
[9] 王泉波.鄂尔多斯盆地南泥湾—临镇地区马六—马五5亚段沉积相与岩相古地理研究[D].西安:西北大学, 2010. WANG Quanbo. Research on the sedimentary facies and lithofacies palaeogeography of Ma55 up to Ma 6 section in area of Nanniwan-Linzhen, Ordos Basin[D]. Xi'an:Northwest University, 2010.
[10] 史基安,邵毅,张顺存,等.鄂尔多斯盆地东部地区奥陶系马家沟组沉积环境与岩相古地理研究[J].天然气地球科学, 2009, 20(3):316-324. SHI Ji'an, SHAO Yi, ZHANG Shuncun, et al. Lithofacies paleogeography and sedimentary environment in Ordovician Majiagou Formation, eastern Ordos Basin[J]. Natural Gas Geoscience, 2009, 20(3):316-324.
[11] 罗军梅.靖边潜台西侧奥陶系马家沟组马五4-马五5储层特征研究[D].武汉:长江大学, 2012. LUO Junmei. Study on reservoir characteristics of Ma 54 and Ma 55 in Ordovician Majiagou Formation in the western side of Jingbian burial platform[D]. Wuhan:Yangtze University, 2012.
[12] 付斯一,陈洪德,苏中堂,等.鄂尔多斯盆地奥陶系马家沟组中组合沉积微相特征及演化[J].中国矿业, 2015, 24(3):81-86. FU Siyi, CHEN Hongde, SU Zhongtang, et al. The characteristic and evolution of sedimentary microfacies in the middle Ordovician assemblages in the Ordos Basin[J]. China Mining Magazine, 2015, 24(3):81-86.
[13] 苏中堂,佘伟,罗静兰,等.鄂尔多斯盆地奥陶系马五5亚段沉积微相与古地理演化[J].沉积学报, 2021, 39(6):1344-1356. SU Zhongtang, SHE Wei, LUO Jinglan, et al. Microfacies and paleogeographic evolution of Ma55 member in the Ordovician, Ordos Basin[J]. Acta Sedimentologica Sinica, 2021, 39(6):1344-1356.
[14] 胡文瑞,翟光明.鄂尔多斯盆地油气勘探开发的实践与可持续发展[J].中国工程科学, 2010, 12(5):64-72. HU Wenrui, ZHAI Guangming. Practice and sustainable development of oil and nature gas exploration and development in Ordos Basin[J]. Strategic Study of CAE, 2010, 12(5):64-72.
[15] 王宝清,章贵松.鄂尔多斯盆地苏里格地区奥陶系古岩溶储层成岩作用[J].石油实验地质, 2006, 28(6):518-522. WANG Baoqing, ZHANG Guisong. Diagenesis of Ordovician paleo karst reservoir in the Sulige area, the Ordos Basin[J]. Petroleum Geology & Experiment, 2006, 28(6):518-522.
[16] 杨华,张军,王飞雁,等.鄂尔多斯盆地古生界含气系统特征[J].天然气工业, 2000, 20(6):7-11. YANG Hua, ZHANG Jun, WANG Feiyan, et al. Characteristics of Paleozoic gas system in Ordos Basin[J]. Natural Gas Industry, 2000, 20(6):7-11.
[17] 郑孟林,金之钧,王毅,等.鄂尔多斯盆地北部中新生代构造特征及其演化[J].地球科学与环境学报, 2006, 28(3):31-36. ZHENG Menglin, JIN Zhijun, WANG Yi, et al. Structural characteristics and evolution of north Ordos Basin in Late Mesozoic and Cenozoic[J]. Journal of Earth Sciences and Environment, 2006, 28(3):31-36.
[18] 姚泾利,赵永刚,雷卞军,等.鄂尔多斯盆地西部马家沟期层序岩相古地理[J].西南石油大学学报(自然科学版), 2008, 30(1):33-38. YAO Jingli, ZHAO Yonggang, LEI Bianjun, et al. Majiagou sequence lithofacies paleogeography in the western Ordos Basin[J]. Journal of Southwest Petroleum University (Science & Technology Edition), 2008, 30(1):33-38.
[19] 周树勋,马振芳.鄂尔多斯盆地中东部奥陶系不整合面成藏组合及其分布规律[J].石油勘探与开发, 1998, 25(5):14-17. ZHOU Shuxun, MA Zhenfang. Study on the play and the distribution of Ordovician unconformity in central-east Ordos Basin[J]. Petroleum Exploration and Development, 1998, 25(5):14-17.
[20] 罗清清,刘波,姜伟民,等.鄂尔多斯盆地中部奥陶系马家沟组五段白云岩储层成岩作用及孔隙演化[J].石油与天然气地质, 2020, 41(1):102-115. LUO Qingqing, LIU Bo, JIANG Weimin, et al. Diagenesis and pore evolution of dolomite reservoir in the 5th member of the Ordovician Majiagou Formation, central Ordos Basin[J]. Oil & Gas Geology, 2020, 41(1):102-115.
[21] 彭军,夏梦,曹飞,等.塔里木盆地顺北一区奥陶系鹰山组与一间房组沉积特征[J].岩性油气藏, 2022, 34(2):17-30. PENG Jun, XIA Meng, CAO Fei, et al. Sedimentary characteristics of Ordovician Yingshan Formation and Yijianfang Formation in Shunbei-1 area, Tarim Basin[J]. Lithologic Reservoirs, 2022, 34(2):17-30.
[22] 冯增昭.华北早奥陶世岩相古地理新探[J].地质科学, 1979(4):302-313. FENG Zengzhao. A preliminary discussion on the Lower Ordovician lithofacies and paleogeography in north China[J]. Scientia Geologica Sinica, 1979(4):302-313.
[23] 李文厚,陈强,李智超,等.鄂尔多斯地区早古生代岩相古地理[J].古地理学报, 2012, 14(1):85-100. LI Wenhou, CHEN Qiang, LI Zhichao, et al. Lithofacies palaeogeography of the Early Paleozoic in Ordos area[J]. Journal of Palaeogeography (Chinese Edition), 2012, 14(1):85-100.
[24] 李峰峰,郭睿,余义常.碳酸盐岩沉积相研究进展[J].科技导报, 2021, 39(8):128-140. LI Fengfeng, GUO Rui, YU Yichang. Progress and prospects of studies of carbonate rock facies[J]. Science & Technology Review, 2021, 39(8):128-140.
[25] 李振清,周洪瑞,陈建强.山东淄博地区上寒武统沉积地球化学特征及其层序地层学意义[J].现代地质, 2001, 15(4):377-382. LI Zhenqing,ZHOU Hongrui,CHEN Jianqiang. Sedimental geochemical characteristics and application of upper Cambrian in Zibo area, Shandong[J]. Geoscience, 2001, 15(4):377-382.
[26] 匡少平,徐仲,张书圣,等.运用地球化学方法研究中、新生代环境气候演替:兼论四川盆地侏罗纪气候变化[J].青岛化工学院学报(自然科学版), 2002, 23(1):4-9. KUANG Shaoping, XU Zhong, ZHANG Shusheng, et al. Applying geochemistry to tesearch into Meso-Cenozoic climate:Discussion on Jurassic climatic change in Sichuan Basin, China[J]. Journal of Qingdao Institute of Chemical Technology (Natural Science Edition), 2002, 23(1):4-9.
[27] 雷国良,王长生,钱志鑫,等.贵州岩溶沉积物稀土元素地球化学研究[J].矿物学报, 1994, 14(3):298-308. LEI Guoliang, WANG Changsheng, QIAN Zhixin, et al. REE geochemistry of karst sediments in Guizhou province[J]. Acta Mineralogica Sinica, 1994, 14(3):298-308.
[28] 金晓辉,张军涛,孙冬胜,等.鄂尔多斯盆地南缘上奥陶统平凉组浅钻中古岩溶洞穴的发现及其意义[J].石油与天然气地质, 2021, 42(3):595-603. JIN Xiaohui, ZHANG Juntao, SUN Dongsheng, et al. Discovery and significance of the Ordovician paleo-karst caves in shallow drilling in the southern Ordos Basin[J]. Oil & Gas Geology, 2021, 42(3):595-603.
[29] 杜江民.苏里格地区奥陶系马家沟组马五5亚段储层特征及其主控因素研究[D].西安:西北大学, 2016. DU Jiangmin. Study on reservoir characteristics and main controlling factors for M55 sub-member of the Ordovician Majiagou Formation in Sulige area[D]. Xi'an:Northwest University, 2016.
[30] 周进高,张帆,郭庆新,等.鄂尔多斯盆地下奥陶统马家沟组障壁潟湖沉积相模式及有利储层分布规律[J].沉积学报, 2011, 29(1):64-71. ZHOU Jingao, ZHANG Fan, GUO Qingxin, et al. Barrierlagoon sedimentary model and reservoir distribution regularity of Lower-Ordovician Majiagou Formation in Ordos Basin[J]. Acta Sedimentologica Sinica, 2011, 29(1):64-71.
[31] 付金华,吴兴宁,孙六一,等.鄂尔多斯盆地马家沟组中组合岩相古地理新认识及油气勘探意义[J].天然气工业, 2017, 37(3):9-16. HU Jinhua, WU Xingning, SUN Liuyi, et al. New understandings of the lithofacies paleogeography of the middle assemblage of Majiagou Fm in the Ordos Basin and its exploration significance[J]. Natural Gas Industry, 2017, 37(3):9-16.
[32] 杨西燕.鄂尔多斯盆地奥陶系马五5亚段白云岩成因及储层主控因素研究[D].成都:成都理工大学, 2018. YANG Xiyan. Origin of dolomite and controlling factor of dolomite reservoir in Ma55 sub-member of Ordovician Majiagou Formation in Ordos Basin[D]. Chengdu:Chengdu University of Technology, 2018.
[33] 包洪平,张云峰,王前平,等.鄂尔多斯盆地马五5亚段沉积微相分布及演化[J].煤田地质与勘探, 2016, 44(5):16-21. BAO Hongping, ZHANG Yunfeng, WANG Qianping, et al. Distribution and evolution of sedimentary microfacies of submember 5 Majiagou Formation in the Ordos Basin[J]. Coal Geology & Exploration, 2016, 44(5):16-21.
[34] 王彦良,王建国,常森,等.苏里格气田东区下奥陶统马五5厚层白云岩储层成因[J].石油地质与工程, 2017, 31(6):20-25. WANG Yanliang, WANG Jianguo, CHANG Sen, et al. Genesis of thick dolomite in the Lower Ordovician Ma 55 in eastern area of the Sulige gas field[J]. Petroleum Geology and Engineering, 2017, 31(6):20-25.
[35] 杜江民,张小莉,聂万才,等.苏里格地区马五5亚段储集层特征及其主控因素[J].新疆石油地质, 2017, 38(1):34-40. DU Jiangmin, ZHANG Xiaoli, NIE Wancai, et al. Study on reservoir characteristics and main controlling factors of M55 submember in Sulige area[J]. Xinjiang Petroleum Geology, 2017, 38(1):34-40.
[36] 王建民,王佳媛.鄂尔多斯盆地伊陕斜坡上的低幅度构造与油气富集[J].石油勘探与开发, 2013, 40(1):49-57. WANG Jianmin, WANG Jiayuan. Low-amplitude structures and oil-gas enrichment on the Yishaan slope, Ordos Basin[J]. Petroleum Exploration and Development, 2013, 40(1):49-57.
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