中国地质调查局成都地质调查中心主办
高级检索

鄂尔多斯盆地合水地区长81亚油层组沉积相及对储层物性的影响

,  ,  ,  , 

文章导航 > 沉积与特提斯地质 > 2021 > 41(1): 88-99

上一篇

下一篇

王茜, 魏凡, 张妍, 范琳, 方一钢. 2021. 鄂尔多斯盆地合水地区长81亚油层组沉积相及对储层物性的影响. 沉积与特提斯地质, 41(1): 88-99. doi: 10.19826/j.cnki.1009-3850.2020.10003
引用本文: 王茜, 魏凡, 张妍, 范琳, 方一钢. 2021. 鄂尔多斯盆地合水地区长81亚油层组沉积相及对储层物性的影响. 沉积与特提斯地质, 41(1): 88-99. doi: 10.19826/j.cnki.1009-3850.2020.10003
shu
Wang Xi, Wei Fan, Zhang Yan, Fan Lin, Fang Yigang. 2021. Sedimentary facies of sub oil-bearing formation of Chang 81 and their influence on physical properties of reservoir, Heshui, Ordos Basin, NW China. Sedimentary Geology and Tethyan Geology, 41(1): 88-99. doi: 10.19826/j.cnki.1009-3850.2020.10003
Citation: Wang Xi, Wei Fan, Zhang Yan, Fan Lin, Fang Yigang. 2021. Sedimentary facies of sub oil-bearing formation of Chang 81 and their influence on physical properties of reservoir, Heshui, Ordos Basin, NW China. Sedimentary Geology and Tethyan Geology, 41(1): 88-99. doi: 10.19826/j.cnki.1009-3850.2020.10003
shu

鄂尔多斯盆地合水地区长81亚油层组沉积相及对储层物性的影响

  • 1. 中国石油天然气股份有限公司长庆油田分公司第十二采油厂, 甘肃 合水 745400;

  • 2. 中国石油天然气股份有限公司长庆油田分公司第二采油厂, 甘肃 庆城 745100;

  • 3. 西南石油大学地球科学与技术学院, 四川 成都 610500;

  • 4. 中国石油天然气股份有限公司长庆油田分公司第十一采油厂, 甘肃 庆阳 745000

  • 基金项目:

    国家科技重大专项子课题中生界低渗透储层非均质性评价技术(2016ZX05050006)

详细信息
    作者简介: 王茜(1995—),女,助理工程师,硕士,主要从事沉积学与储层地质学研究。E-mail:466277231@qq.com

  • 中图分类号: P534.51;TE122

Sedimentary facies of sub oil-bearing formation of Chang 81 and their influence on physical properties of reservoir, Heshui, Ordos Basin, NW China

  • 1. The 12th Oil Production Plant, Changqing Oilfield Company, PetroChina, Heshui, 745400, China;

  • 2. The 2nd Oil Production Plant, Changqing Oilfield Company, PetroChina, Qingcheng, 745100, China;

  • 3. School of Geoscience and Technology, Southwest Petroleum University, Chengdu, 610500, China;

  • 4. The 11th Oil Production Plant, Changqing Oilfield Company, PetroChina, Qingyang, 745000, China

    摘要
  • 为研究鄂尔多斯盆地上三叠统延长组长81亚油层组沉积微相与储层物性的关系，通过岩心相、测井相及物性等资料，结合前人研究成果，对盆内合水地区长81亚油层组进行分析。认为：（1）长81亚油层组浅水三角洲前缘沉积发育水下分流河道、河口坝、前缘席状砂、分流间湾4种沉积微相。多期叠置的水下分流河道是控制砂体发育的主要微相类型，根据砂地比又可分为河道核部、河道中部及河道侧翼；（2）长812小层水下分流河道砂体发育频率较高、沉积期次较多、连通性较强，其次为长811小层与长813小层；（3）由沉积微相决定的岩石结构成熟度控制了储层的初始孔隙度，进而在一定程度上影响了储层现今孔隙度。水下分流河道核部储层物性最好，是有利微相类型。研究区长812小层有利微相发育规模最大，为后期勘探开发首要目的层位。
    Basing on the data of drilling cores, logging records and testing of physical properties of reservoir, this paper discusses the relationship between sedimentary microfacies and reservoir physical properties of the sub oil-formation of Chang 81of the Upper Triassic Yanchang Formation in Ordos Basin.Four types of microfacies, including underwater distributary channel, mouth bar, frontal sheet sand and inter-distributary bay, occur in the sub oil-formationof Chang 81, which is with sedimentary facies of shallow delta front. The multi-stage superimposed underwater distributary channel is the main type of microfacies controlling the development of sand bodies. According to its thickness ratios of sandstone and mudstone, it can be divided into the core, the middle and the flank of the channel.The subaqueous distributary channels occur frequently in small layers of Chang 812, whose sedimentary periods are more often than Chang 811 and Chang 813,and its connectivity is better.The structural maturity, which is determined by sedimentary microfacies, controls the initial porosity of the reservoir and then affects the current porosity of the reservoir to a certain extent. The reservoir in the core of underwater distributary channel is with the best physical properties, and it is the favorable microfacies type. It is suggested that the small layers of Chang 812, is the potential target layers for future exploration in studied areas.
    • HTML全文
  • 加载中
    • 参考文献(33)

  • [1] 焦方正.非常规油气之"非常规"再认识[J].石油勘探与开发,2019,46(5):803-810.

    [2] 王正和,余谦.准南上二叠统芦草沟组非常规油气储层特征[J].岩性油气藏,2017,29(5):28-35.

    [3] 宋岩,李卓,姜振学,等.非常规油气地质研究进展与发展趋势[J].石油勘探与开发,2017,44(4):638-648.

    [4] 张航,廖明光,姚泾利,等.致密砂岩储层自生矿物特征及其对储集性能的影响——以鄂尔多斯盆地陇东地区长3油组为例[J].沉积与特提斯地质,2017,37(3):22-31.

    [5] CuiJ W,Li S,Mao Z G. Oil-bearing heterogeneity and threshold of tight sandstone reservoirs:A case study on Triassic Chang7 member,Ordos Basin[J].Marine and Petroleum Geology,2019,104(6):180-189.

    [6] Li C Z,Wang H H,Wang L G,et al. Characteristics of tight oil sandstone reservoirs:A case study from the Upper Triassic Chang 7 Member in Zhenyuan area,Ordos Basin,China[J].Arabian Journal of Geoscience 2020,13(2):23-35.

    [7] Qiao J C,Zeng J H,Jiang S,et al. Impacts of sedimentology and diagenesis on pore structure and reservoir quality in tight oil sandstone reservoirs:Implications for macroscopic and microscopic heterogeneities[J]. Marine and Petroleum Geology,2020,111(1):279-300.

    [8] Zhong Y J,Huang K K,Ye L M,et al. Diagenesis of tight sandstone reservoirs of Xujiahe Formation (Upper Triassic) the Xinchang Gas Field,western Sichuan Basin,China[J]. Geological Journal,2020,55(6):4604-4624.

    [9] Hoy R G,Ridgway K D. Sedimentology and sequence stratigraphy of fan-delta and river-delta depo-systems,Pennsylvanian Minturn Formation,Colorado[J]. AAPG bulletin,2003,87(7):1169-1191.

    [10] Li Y J,Zhao Y,Yang R C,et al. Detailed sedimentary facies of a sandstone reservoir in the eastern zone of the Sulige gas field,Ordos Basin[J]. Mining Science and Technology (China),2010,20(11)891-897+903.

    [11] 李思田.沉积盆地分析中的沉积体系研究[J]. 矿物岩石地球化学,1988,7(2):90-92.

    [12] 李璟,傅强,邓秀琴,等.李祥同.鄂尔多斯盆地华池-庆阳地区延长组长62-63沉积微相研究[J].沉积与特提斯地质,2018,38(4):68-75.

    [13] 陆金波,王英民,张雷,等.塔河九连片地区三叠系下油组砂体分布及有利区带预测[J].沉积与特提斯地质,2011,31(1):53-58.

    [14] 冯旭东,张东,林春明,等.松辽盆地白垩系浅水湖泊三角洲沉积微相研究-以大庆杏树岗油田杏三区东部葡Ⅰ1-3小层为例[J].沉积与特提斯地质,2016,36(2):1-10.

    [15] 李士祥,楚美娟,黄锦绣,等.鄂尔多斯盆地延长组长8油层组砂体结构特征及成因机理[J].石油学报,2013,34(3):435-444.

    [16] 曹江骏,杨友运,陈朝兵,等.致密砂岩储层骨架砂体构型特征-以鄂尔多斯盆地合水地区延长组长6段砂体为例[J].沉积学报,2019,37(6):1105-1116+1103.

    [17] 王朋岩,李耀华.松辽盆地中央坳陷朝84-6井区泉头组四段沉积期双物源体系分析[J].沉积与特提斯地质,2016,36(1):90-97.

    [18] 李鹏飞,徐论勋,李建明.鄂尔多斯盆地华庆地区长6期物源分析[J].沉积与特提斯地质,2010,30(2):61-65.

    [19] 杨友运,张蓬勃,张忠义.鄂尔多斯盆地合水油田长8油组辫状河三角洲沉积特征与层序演化[J].地质科技情报,2005,24(1):45-48.

    [20] 司学强,张金亮.合水油田长8油组沉积相与油气分布规律[J].西南石油大学学报(自然科学版),2008,30(6):67-71+208.

    [21] 刘强.合水东侧西127-板10砂带长8沉积特征及有利区筛选[D].西安:西北大学,2016.

    [22] 李德生.重新认识鄂尔多斯盆地油气地质学[J]. 石油勘探与开发,2004,31(6):1-7.

    [23] 李文厚,刘溪,张倩,等.鄂尔多斯盆地中晚三叠世延长期沉积演化[J].西北大学学报(自然科学版),2019,49(4):605-621.

    [24] 王一帆,徐胜林,张兵,等.川西坳陷西充-梓潼地区下沙溪庙组沉积微相特征[J].沉积与特提斯地质,2020,40(1):35-44.

    [25] 李元昊,刘池洋,独育国,等.鄂尔多斯盆地西北部上三叠统延长组长8油层组浅水三角洲沉积特征及湖岸线控砂[J].古地理学报,2009,11(3):265-274.

    [26] 叶蕾,朱筱敏,秦祎,等.断陷湖盆浅水三角洲沉积体系[J].地球科学与环境学报,2018,40(2):186-202.

    [27] Purkait B,Majumdar D D. Distinguishing different sedimentary facies in a deltaic system[J]. Sedimentary Geology,2014,308(7):53-62.

    [28] 罗静兰,李忠兴,史成恩,等. 鄂尔多斯盆地西南部上三叠统延长组长8、长6油层组的沉积体系与物源方向[J]. 地质通报,2008,27(1):101-111.

    [29] 罗静兰,史成恩,李博,等.鄂尔多斯盆地周缘及合水地区延长组长8、长6沉积物源-来自岩石地球化学的证据[J].中国科学(D辑:地球科学),2007,37(S1):62-72.

    [30] 陈林,陆永潮,林卫兵,等.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(04):434-447.

    [31] Beard D C,Weyl P K. Influence of texture on porosity and permeabilityof unconsolidated Sand[J].AAPG Bulletin,1973,57(2):349-369.

    [32] 杨勇,黄有根,冯炎松,等.致密砂岩填隙物特征及其对储层的影响[J].西南石油大学学报(自然科学版),2015,37(5):1-8.

    [33] 李志鹏.甘肃合水地区庄36井区地层划分、对比及沉积相研究[D].北京:中国地质大学(北京),2011.

    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
计量
  • 文章访问数:  833
  • PDF下载数:  68
  • 施引文献:  0
出版历程
收稿日期:  2020-08-07
修回日期:  2020-10-24

目录

    版权所有：中国地质调查局发展研究中心 copyright @2020
    返回