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张家湾地区长_7页岩生烃潜力及孔隙结构特征
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  • 英文篇名:Hydrocarbon Generation Potential and Pore Characteristics of Chang 7 Oil Shale in the Zhangjiawan Region
  • 作者:唐建云 ; 张刚 ; 樊宏伟 ; 刘见通 ; 陈玉宝
  • 英文作者:TANG Jianyun;ZHANG Gang;FAN Hongwei;LIU Jiantong;CHEN Yubao;Department of Petroleum Engineering of Karamay Vocational and Technical College;China University of Petroleum (Beijing) Karamay Campus;Dingbian Oil Factory of Yanchang Petroleum Co.Ltd.;Yanchang Petroleum Co.Ltd.;
  • 关键词:页岩 ; 生烃潜力 ; 孔隙特征 ; 长_7 ; 直罗油田
  • 英文关键词:shale;;potential of hydrocarbon generation;;pore characteristics;;Chang 7;;Zhiluo Oilfield
  • 中文刊名:XNSY
  • 英文刊名:Journal of Southwest Petroleum University(Science & Technology Edition)
  • 机构:克拉玛依职业技术学院;中国石油大学(北京)克拉玛依校区;延长油田股份有限公司定边采油厂;延长油田股份有限公司;
  • 出版日期:2019-03-19 09:39
  • 出版单位:西南石油大学学报(自然科学版)
  • 年:2019
  • 期:v.41;No.194
  • 基金:新疆维吾尔自治区自然科学基金(2017D01B56)
  • 语种:中文;
  • 页:XNSY201903003
  • 页数:13
  • CN:03
  • ISSN:51-1718/TE
  • 分类号:32-44
摘要
为了摸清直罗油田张家湾地区延长组长_7页岩生烃潜力及孔隙特征,过岩石学、有机地球化学分析以及利用扫描电镜、氩离子抛光等技术手段,对研究区长_7页岩进行了展布特征、地球化学特征和孔隙特征分析。结果表明,研究区延长组长_7段黑色湖相页岩在平面上和纵向上均存在差异,具有"北西厚、南东薄"的特征;长_7油页岩有机质类型以Ⅰ型和Ⅱ_1型为主,有机质成熟度高,为好的烃源岩,页岩储层属于Ⅰ类富集型储层;孔隙类型以粒间孔、晶间孔、溶蚀孔和有机质孔为主;孔径以<0.5μm为主,储层喉道半径主要在100~750 nm,孔隙度变化范围较大,主要在0.5%~1.9%,平均约1.0%。研究认为,研究区"新发现"的长_7页岩生烃潜力较大,可动油含量较高。
        Hydrocarbon generation potential and pore characteristics of Chang 7 oil shale from the Yanchang Formation in the Zhangjiawan Region of the Zhiluo Oilfield were examined in this study. We conducted petrological and organic geochemical analyses, and methods like scanning electron microscopy and argon ion milling were used to analyze the distribution, geochemical characteristics, and pore characteristics of the Chang 7 shale in the study area. The results reveal that the Chang 7 black lake shale from the Yanchang Formation in the study area is heterogeneous both horizontally and vertically. It is thick in the northwest, but thin in the southeast. The organic matter in the Chang 7 oil shale are primarily type Ⅰ and Ⅱ_1 and are highly mature. Therefore, the shale is a desirable hydrocarbon source rock. The shale reservoir is a type 1 enrichment reservoir. The pores of the reservoir are mainly intergranular pores, intercrystalline pores, dissolution pores, and organic pores, where the pore sizes are mostly <0.5 μm. The throat radius ranges from 100 to 750 nm. There is a relatively porosity range(0.5% to 1.9%)with an average of approximately 1.0%. It is believed that the"newly discovered"Chang 7 shale in the study area has relatively great hydrocarbon generation potential, with a relatively high content of movable oil.
引文
[1]杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京:石油工业出版社,2002.YANG Junjie. Tectonic evolution and petroleum distribution of Ordos Basin[M]. Beijing:Petroleum Industry Press, 2002.
    [2]赵澄林,朱筱敏.沉积岩石学[M].北京:石油工业出版社,2001.ZHAO Chenglin, ZHU Xiaomin. Sedimentary petrography[M]. Beijing:Petroleum Industry Press, 2001.
    [3]何自新.鄂尔多斯盆地演化与油气[M].北京:石油工业出版社,2003.HE Zixin. The evolution and petroleum of the Ordos Basin[M]. Beijing:Petroleum Industry Press, 2003.
    [4]袁选俊,林森虎,刘群,等.湖盆细粒沉积特征与富有机质页岩分布模式——以鄂尔多斯盆地延长组长7油层组为例[J].石油勘探与开发,2015, 42(1):34-43.doi:10.11698/PED.2015.01.04YUAN Xuanjun, LIN Senhu, LIU Qun, et al. Lacustrine fine-grained sedimentary features and organic-rich shale distribution pattern:A case study of Chang 7 Member of Triassic Yanchang Formation in Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2015,42(1):34-43. doi:10.11698/PED.2015.01.04
    [5]李玉宏,姜亭,武富礼,等.鄂尔多斯盆地东南部油页岩资源评价[J].地质报,2014, 33(9):1417-1424.LI Yuhong, JIANG Ting, WU Fuli, et al. Evaluation methods and results of oil shale resources in southeastern Ordos Basin[J]. Geological Bulletin of China, 2014, 33(9):1417-1424.
    [6]徐勇,胡士骏,陈国俊,等.鄂尔多斯盆地东南部延长组长7段页岩孔隙特征与吸附能力[J].岩性油气藏,2016,28(6):30-35. doi:10.3969/j.issn.1673-8926.-2016.06.005XU Yong, HU Shijun, CHEN Guojun, et al. Pore characteristics and adsorption capacity of Chang 7 shale of Yanchang Formation in the southeastern Ordos Basin[J].Lithologic Reservoirs, 2016,28(6):30-35. doi:10.3969/j.-issn.1673-8926.2016.06.005
    [7]耳闯,罗安湘,赵靖舟,等.鄂尔多斯盆地华池地区三叠系延长组长7段富有机质页岩岩相特征[J].地学前缘,2016,23(2):108-117. doi:10.13754/j.esf.2016.02.011ER Chuang, LUO Anxiang, ZHAO Jingzhou, et al. Lithofacies features of organic rich shale of the Triassic Yanchang Formation in Huachi Area, Ordos Basin[J]. Earth Science Hrontiers, 2016,23(2):108-117.doi:10.13754/j.-esf.2016.02.011
    [8]张文正,杨华,杨伟伟,等.鄂尔多斯盆地延长组长7湖相页岩油地质特征评价[J].地球化学,2015,44(5):505-515. doi:10.19700/j.0379-1726.2015.05.010ZHANG Wenzheng,YANG Hua,YANG Weiwei,et al.Assessment of geological characteristics of lacustrine shale oil reservoir in Chang 7 Member of Yanchang Formation, Ordos Basin[J]. Geochimica, 2015, 44(5):505-515. doi:10.19700/j.0379-1726.2015.05.010
    [9]王香增,高胜利,高潮.鄂尔多斯盆地南部中生界陆相页岩气地质特征[J].石油勘探与发,2014, 41(3):294-304. doi:10.11698/PED.2014.03.04WANG Xiangzeng, GAO Shengli, GAO Chao. Geological features of Mesozoic continental shale gas in south of Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2014,41(3):294-304. doi:10.11698/PED.-2014.03.04
    [10]高岗,刘显阳,王银会,等.鄂尔多斯盆地陇东地区长7段页岩油特征与资源潜力[J].地学前缘,2013,20(2):140-146.GAO Gang, LIU Xianyang, WANG Yinhui, et al. Characteristics and resource potential of the oil shale of Chang7 Layer in Longdong Area, Ordos Basin[J]. Earth Science Frontiers, 2013, 20(2):140-146.
    [11]杨华,李士祥,刘显阳.鄂尔多斯盆地致密油、页岩油特征及资源潜力[J].石油学报,2013,34(1):1-11. doi:10.7623/syxb201301001YANG Hua, LI Shixiang, LIU Xianyan. Characteristics and resource prospects of tight oil and shale oil in Ordos Basin[J]. Acta Petrolei Sinica, 2013, 34(1):1-11. doi:10.-7623/syxb201301001
    [12]杨华,牛小兵,徐黎明,等.鄂尔多斯盆地三叠系长7段页岩油勘探潜力[J].石油勘探与开发,2016, 43(4):511-520. doi:10.11698/PED.2016.04.02YANG Hua, NIU Xiaobing, XU Liming, et al. Exploration potential of shale oil in Chang 7 Member, upper Triassic Yanchang Formation, Ordos Basin, NW China[J].Petroleum Exploration and Development, 2016, 43(4):511-520. doi:10.11698/PED.2016.04.02
    [13]刘岩,周文,邓虎成.鄂尔多斯盆地上三叠统延长组含气页岩地质特征及资源评价[J].天然气工业,2013,33(3):19-23. doi:10.3787/j.issn.1000-0976.-2013.03.005LIU Yar, ZHOU Wen, DENG Hucheng. Geological characteristics of gas-bearing shales in the Yanchang Formation and its resource assessment in the Ordos Basin[J].Natural Gas Industry, 2013, 33(3):19-23. doi:10.3787/j.-issn.1000-0976.2013.03.005
    [14]唐建云,王志维,也尔哈那提·黑扎提,等.鄂尔多斯盆地旬邑探区延长组烃源岩及原油地球化学特征[J].岩性油气藏,2017, 29(2):107-116. doi:10.3969/j.issn.-1673-8926.2017.02.013TANG Jianyun, WANG Zhiwei, YE'ERHANATI Heizhati, et al. Source rocks and geochemical characteristics of crude oil of the Yanchang Formation in Xunyi exploration Area,Ordos Basin[J]. Lithologic Reservoirs,2017, 29(2):107-116. doi:10.3969/j.issn.1673-8926.2017.02.013
    [15]邓南涛,张枝焕,任来义,等.鄂尔多斯盆地南部延长组油页岩地球化学特征及分布规律[J].石油实验地质,2013,35(4):432-437. doi:10.11781/sysydz201304432DENG Nantao, ZHANG Zhihuan, REN Laiyi, et al. Geochemical characteristics and distribution rules of oil shale from Yanchang Formation, Southern Ordos Basin[J]. Petroleum Geology&Experiment, 2013, 35(4):432-437.doi:10.11781/sysydz201304432
    [16]唐建云,史政,宋红霞,等.富黄探区延长组烃源岩评价与油源对比[J].西南石油大学学报(自然科学版),2016, 38(3):11-20. doi:10.11885/j.issn.1674-5086.2015.10.20.01TANG Jianyun, SHI Zheng, SONG Hongxia, et al. Hydrocarbon source evaluation and oil source contrast of the Yanchang Formation in Fu-Huang exploration area, Ordos Basin[J]. Journal of Southwest Petroleum University(Science&Technology Edition),2016, 38(3):11-20. doi:10.11885/j.issn.1674-5086.2015.10.20.01
    [17] PRICE L C, BARKER C E. Suppression of vitrinite reflectance in amorphous rich kerogen:A major unrecognized problem[J]. J. Petrol. Geol., 1985, 8(1):59-84. doi:10.1111/j.1747-5457.1985.tb00191.x
    [18]王铁冠,钟宁宁,熊波,等.源岩生烃潜力的有机岩石学评价方法[J].石油学报,1994, 15(4):9-16.WANG Tieguan, ZHONG Ningning, XIONG Bo, et al. Organic petrologic methodology for evaluation of hydrocarbon generation potential in source rocks[J]. Acta Petrolei Sinica, 1994, 15(4):9-16.
    [19]卢双舫,黄文彪,陈方文,等.页岩油气资源分级评价标准探讨[J].石油勘探与开发,2012, 39(2):249-256.LU Shuangfang, HUANG Wenbiao, CHEN Fangwen, et al. Classification and evaluation criteria of shale oil and gas resources:Discussion and application[J]. Petroleum Exploration and Development, 2012, 39(2):249-256.
    [20]吴松涛,邹才能,朱如凯,等.鄂尔多斯盆地上三叠统长7段泥页岩储集性能[J].地球科学(中国地质大学学报),2015, 40(11):1810-1823. doi:10.3799/dqkx.-2015.162WU Songtao, ZOU Caineng, ZHU Rukai, et al. Reservoir characterization of upper Triassic Chang 7 shale in Ordos Basin[J]. Earth Science(Journal of China University of Geosciences), 2015, 40(11):1810-1823. doi:10.-3799/dqkx.2015.162
    [21]曾秋楠,于炳松,李昱霏.鄂尔多斯盆地东南部延长组页岩储层特征及控制因素[J].特种油气藏,2013,20(1):23-26. doi:10.3969/j.issn.1006-6535.2013.01.-006ZENG Qiunan, YU Bingsong, LI Yufei. Reservoir characteristics and control factors in the shale bed of Yanchang Formation of southeast in Ordos Basin[J]. Special Oil and Gas Reservoir, 2013, 20(1):23-26. doi:10.3969/j.issn.-1006-6535.2013.01.006
    [22]王香增,张丽霞,李宗田,等.鄂尔多斯盆地延长组陆相页岩孔隙类型划分方案及其油气地质意义[J].石油与天然气地质,2016,37(1):1-7.doi:10.-11743/ogg20160101WANG Xiangzeng,ZHANG Lixia,LI Zongtian, et al.Pore type classification scheme for continental Yanchang shale in Ordos Basin and its geological significance[J]. Oil&Gas Geology, 2016, 37(1):1-7. doi:10.-11743/ogg20160101
    [23]熊健,罗丹序,刘向君,等.鄂尔多斯盆地延长组页岩孔隙结构特征及其控制因素[J].岩性油气藏,2016,28(2):16-23. doi:10.3969/j.issn.1673-8926.2016.02.-003XIONG Jian, LUO Danxu, LIU Xiangjun, et al. Characteristics and controlling factors of shale pore structure of Yanchang Formation in Ordos Basin[J]. Lithologic Reservoirs, 2016,28(2):16-23. doi:10.3969/j.issn.1673-8926.-2016.02.003
    [24]张烨毓,周文,唐瑜,等.鄂尔多斯盆地三叠系长7油层组页岩储层特征[J].成都理工大学学报(自然科学版),2013,40(6):671-676. doi:10.3969/j.issn. 1671-9727.2013.06.06ZHANG Yeyu, ZHOU Wen, TANG Yu, et al. Characteristics of shale reservoir rocks in Member 7 of Triassic Yanchang Formation in Ordos Basin, China[J]. Journal of Chengdu University of Technology(Science&Technology Edition), 2013,40(6):671-676. doi:10.3969/j.issn.-1671-9727.2013.06.06
    [25]吴松涛,朱如凯,崔京钢,等.鄂尔多斯盆地长7湖相泥页岩孔隙演化特征[J].石油勘探与开发,2015,42(2):167-176. doi:10.11698/PED.2015.02.05WU Songtao, ZHU Rukai, CUI Jinggang, et al. Character-istics of lacustrine shale porosity evolution, Triassic Chang7 Member, Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2015, 42(2):167-176. doi:10.-11698/PED.2015.02.05
    [26]俞雨溪,罗晓容,雷裕红,等.陆相页岩孔隙结构特征研究——以鄂尔多斯盆地延长组页岩为例[J].天然气地球科学,2016,27(4):716-726. doi:10.11764/j.issn.-1672-1926.2016.04.0716YU Yuxi, LUO Xiaorong, LEI Yuhong, et al. Characterization of lacustrine shale pore structure:An example from the upper Triassic Yanchang Formation, Ordos Basin[J].Natural Gas Geoscience, 2016, 27(4):716-726. doi:10.-11764/j.issn. 1672-1926.2016.04.0716
    [27]闫德宇,黄文辉,张金川.鄂尔多斯盆地海陆过渡相富有机质泥页岩特征及页岩气意义[J].地学前缘,2015,22(6):197-206. doi:10.13745/j.esf.2015.06.015YAN Deyu, HUANG Wenhui, ZHANG Jinchuan. Characteristics of marine-continental transitional organic-rich shale in the Ordos Basin and its shale gas significance[J].Earth Science Frontiers, 2015, 22(6):197-206. doi:10.-13745/j.esf.2015.06.015
    [28]曾维特,张金川,丁文龙,等.延长组页岩储层纳米级孔隙特征及影响因素——以鄂尔多斯盆地柳坪171井为例[J].煤炭学报,2014, 39(6):1118-1126. doi:10.-13225/j.cnki.jccs.2013.0842ZENG Weite, ZHANG Jinchuan, DING Wenlong, et al.Characteristic and influence factors of nanopores in Yanchang shale reservoir:A case study of Liuping-171 Well in Ordos Basin[J]. Journal of China Coal Society,2014,39(6):1118-1126. doi:10.13225/j.cnki.jccs.2013.0842
    [29]杨超,张金川,唐玄.鄂尔多斯盆地陆相页岩微观孔隙类型及对页岩气储渗的影响[J].地学前缘,2013,20(4):240-250.YANG Chao, ZHANG Jinchuan, TANG Xuan. Microscopic pore types and its impact on the storage and permeability of continental shale gas, Ordos Basin[J]. Earth Science Hrontiers, 2013, 20(4):240-250.

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