岩性油气藏 ›› 2022, Vol. 34 ›› Issue (2): 17–30.doi: 10.12108/yxyqc.20220202

• 地质勘探 • 上一篇    下一篇

塔里木盆地顺北一区奥陶系鹰山组与一间房组沉积特征

彭军1,2, 夏梦1, 曹飞3, 夏金刚1, 李峰3   

  1. 1. 西南石油大学 地球科学与技术学院, 成都 610500;
    2. 天然气地质四川省重点实验室, 成都 610500;
    3. 中国石化西北油田分公司 勘探开发研究院, 乌鲁木齐 830000
  • 收稿日期:2021-12-06 修回日期:2021-12-23 出版日期:2022-03-01 发布日期:2022-03-14
  • 通讯作者: 夏梦(1995-),女,西南石油大学在读硕士研究生,研究方向为沉积学。Email:593098239@qq.com。 E-mail:593098239@qq.com
  • 作者简介:彭军(1968-),男,博士,教授,博士生导师,主要从事沉积学、储层地质学及层序地层学方面的教学和研究工作。地址:(610500)四川省成都市新都区新都大道8号。Email:445371976@qq.com
  • 基金资助:
    四川省科技厅区域创新合作项目“复杂油藏高效开发相关技术研究及推广应用”（编号：2021YFQ0048）资助

Sedimentary characteristics of Ordovician Yingshan Formation and Yijianfang Formation in Shunbei-1 area, Tarim Basin

PENG Jun1,2, XIA Meng1, CAO Fei3, XIA Jingang1, LI Feng3   

  1. 1. School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China;
    2. Sichuan Key Laboratory of Natural Gas Geology, Chengdu 610500, China;
    3. E Research Institute of Exploration and Development, Sinopec Northwest Oilfield Branch, Urumqi 830000, China
  • Received:2021-12-06 Revised:2021-12-23 Online:2022-03-01 Published:2022-03-14

PDF (PC)

229

摘要： 近年来，塔里木盆地顺北地区油气藏的持续发现揭示了其较大的勘探潜力。通过开展岩心观察、薄片鉴定、常规测井曲线和成像测井图像分析以及元素地球化学测试，对顺北一区奥陶系鹰山组上段与一间房组沉积环境进行了分析，结合沉积相识别标志，系统描述了研究区沉积特征，指明了优质储层类型及有利发育区。研究结果表明：①顺北一区奥陶系鹰山组上段与一间房组Mn的质量分数大于200×10-6，Sr/Ba平均值为2.025 4~3.260 2，U/Th平均值为2.02，多大于0.75，δU平均值为1.29，多大于1，显示沉积时整体处于水体由深变浅、盐度正常、温暖潮湿的弱氧化-弱还原的海相沉积环境。②研究区奥陶系鹰山组上段与一间房组为开阔台地相沉积，发育台坪和台内滩2种亚相，可细分为灰坪、云灰坪、云坪、砂屑滩、生屑滩、颗粒滩等6个微相。③研究区整体以灰坪微相为主，纵向上一间房组砂屑滩与生屑滩微相较鹰山组上段更为发育，平面上自东向西台内滩亚相发育减弱。

关键词: 开阔台地, 海相, 鹰山组上段, 一间房组, 奥陶系, 顺北一区, 塔里木盆地

Abstract: In recent years, the continuous discovery of oil and gas reservoirs in Shunbei area of Tarim Basin reveals its great exploration potential.Through core observation, thin section identification, conventional logging curves and imaging logging image analysis and element geochemistry test, the sedimentary environment of the upper member of Yingshan Formation and Yijianfang Formation of Ordovician(O1-2y-O2yj) in Shunbei-1 area was analyzed. Combined with the identification marks of sedimentary facies, the sedimentary characteristics of the study area were described, and the high-quality reservoir types and favorable reservoir development areas were pointed out. The results show that:(1) The mass fraction of Mn of the upper member of Yingshan Formation and Yijianfang Formation of Ordovician in Shunbei-1 area 1 is greater than 200×10-6, the average value of Sr/BA is 2.025 4-3.260 2, and the average value of U/Th is 2.02, mostly greater than 0.75, the average value of δU is 1.29, mostly greater than 1, which shows that the whole study area was in a marine sedimentary environment with water depth changing from deep to shallow, normal salinity, warm and humid weak oxidation-weak reduction.(2) The upper member of Yingshan Formation and Yijianfang Formation of Ordovician in the study area is an open platform facies deposit, with two subfacies developed:platform flat and intra-platform shoal, and six microfacies, such as limestone flat, dolomite-limestone flat, dolomite flat, sandy debris shoal, bioclastic shoal and granular beach.(3) As a whole, the study area is mainly dominated by limestone flat microfacies.In the vertical direction, the sandy debris shoal and bioclastic shoal microfacies are more developed in Yijianfang Formation than in the upper member of Yingshan Formation.The development of intra-platform shoal subfacies is weakened from east to west in the plane.

Key words: open platform, marine, upper member of Yingshan Formation, Yijianfang Formation, Ordovician, Shunbei-1 area, Tarim Basin

中图分类号: 

  • TE122
[1] 徐梅桂, 贺勇, 范筱聪, 等.塔里木盆地中-下奥陶统层序地层研究[J].新疆地质, 2012, 30(4):404-410.XU Meigui, HE Yong, FAN Xiaocong, et al.The study on LowerMiddle Ordorician stratigraphic sequence in Tarim Basin[J].Xinjiang Geology, 2012, 30(4):404-410.
[2] WILSON A O.Carbonate reservoirs-Porosity evolution and diagenesis in a sequence stratigraphic framework[J].Journal of Petroleum Science and Engineering, 2003, 40(3/4):191-193.
[3] LU Xinbian, WANG Yan, TIAN Fei, et al.New insights into the carbonate karstic fault system and reservoir formation in the southern Tahe area of the Tarim Basin[J].Marine and Petroleum Geology, 2017, 86:587-605.
[4] 李宗杰, 王鹏, 陈绪云, 等.塔里木盆地顺南地区超深白云岩储层地震、地质综合预测[J].石油与天然气地质, 2020, 41(1):59-67.LI Zongjie, WANG Peng, CHEN Xuyun, et al.Integrated seismic and geological prediction of ultra-deep dolomite reservoir in Shunnan area, Tarim Basin[J].Oil&Gas Geology, 2020, 41(1):59-67.
[5] 林波, 张旭, 况安鹏, 等.塔里木盆地走滑断裂构造变形特征及油气意义:以顺北地区1号和5号断裂为例[J].石油学报, 2021, 42(7):906-923.LIN Bo, ZHANG Xu, KUANG Anpeng, et al.Structural deformation characteristics of strike-slip faults in Tarim Basin and their hydrocarbon significance:A case study of No.1 fault and No.5 fault in Shunbei area[J].Acta Petrolei Sinica, 2021, 42(7):906-923.
[6] 林波, 云露, 李海英, 等.塔里木盆地顺北5号走滑断层空间结构及其油气关系[J].石油与天然气地质, 2021, 42(6):1344-1353.LIN Bo, YUN Lu, LI Haiying, et al.Spatial structure of Shunbei No.5 strike-slip fault and its relationship with oil and gas reservoirs in the Tarim Basin[J].Oil&Gas Geology, 2021, 42(6):1344-1353.
[7] 王文博, 傅恒, 闾廖然, 等.塔里木盆地顺北地区奥陶系碳酸盐岩层序模式及其意义[J].沉积学报, 2021, 39(6):1451-1465.WANG Wenbo, FU Heng, LYU Liaoran, et al.Sequence model of Ordovician carbonate strata in Shunbei area, Tarim Basin, and its significance[J].Acta Sedimentologica Sinica, 2021, 39(6):1451-1465.
[8] 陈坤.塔里木盆地顺托果勒中下奥陶统储层发育控制因素研究[D].北京:中国石油大学(北京), 2020.CHEN Kun.Analysis on the reservoir development controlling factors of the Lower and Middle Ordovician in the Shuntuoguole area of the Tarim Basin[D].Beijing:China University of Petroleum (Beijing), 2020.
[9] 王素英, 张翔, 田景春, 等.塔里木盆地顺北地区柯坪塔格组沉积演化及沉积分异模式[J].岩性油气藏, 2021, 33(5):81-94.WANG Suying, ZHANG Xiang, TIAN Jingchun, et al.Sedimentary evolution and sedimentary differentiation model of Kepingtage Formation in Shunbei area, Tarim Basin[J].Lithologic Reservoirs, 2021, 33(5):81-94.
[10] 陈代钊, 钱一雄.深层-超深层白云岩储集层:机遇与挑战[J].古地理学报, 2017, 19(2):187-196.CHEN Daizhao, QIAN Yixiong.Deep or super-deep dolostone reservoirs:Opportunities and challenges[J].Journal of Palaeogeography (Chinese Edition), 2017, 19(2):187-196.
[11] 王天宇, 焦存礼, 杨锋杰, 等.顺南地区中奥陶统一间房组沉积微相特征与展布规律研究[J].山东科技大学学报(自然科学版), 2018, 37(4):12-21.WANG Tianyu, JIAO Cunli, YANG Fengjie, et al.Research on sedimentary microfacies features and distribution law of Middle Ordvician Yijianfang Formation in Shunnan area[J].Journal of Shandong University of Science and Technology (Natural Science), 2018, 37(4):12-21.
[12] 赵锐, 赵腾, 李慧莉, 等.塔里木盆地顺托果勒地区中下奥陶统鹰山组与一间房组沉积相与旋回地层[J].东北石油大学学报, 2019, 43(4):1-16.ZHAO Rui, ZHAO Teng, LI Huili, et al.Sedimentary facies and cyclic stratigraphy of Yingshan and Yijianfang formations of Lower-Middle Ordovician in Shuntuoguole area, Tarim Basin[J].Journal of Northeast Petroleum University, 2019, 43(4):1-16.
[13] 许大钊.顺北地区奥陶系储层成因机制研究[D].成都:西南石油大学, 2018.XU Dazhao.Study on genetic mechanism of Ordovician reservoir in Shunbei area[D].Chengdu:Southwest Petroleum University, 2018.
[14] 王玉伟.顺托果勒地区奥陶系储层多成因形成机制及对油气充注的控制作用[D].武汉:中国地质大学, 2019.WANG Yuwei.Multiple original mechanisms of the Ordovician reservoir and their control on hydrocarbon charging in Shuntuoguole area, Tarim Basin[D].Wuhan:China University of Geosciences, 2019.
[15] 肖玮绮.塔里木盆地顺托果勒低隆起奥陶系鹰山组沉积微相特征[D].成都:成都理工大学, 2019.XIAO Weiqi.Sedimentary microfacies characteristics of Ordovician Yingshan Formation in Shuntuoguole lower uplift, Tarim Basin[D].Chengdu:Chengdu University of Technology, 2019.
[16] 隋欢.顺北地区中下奥陶统储层成岩作用及演化研究[D].成都:西南石油大学, 2019.SUI Huan.Diagenesis and evolution of Middle and Lower Ordovician reservoirs in Shunbei area[D].Chengdu:Southwest Petroleum University, 2019.
[17] 李映涛, 白晓亮, 苏炳睿, 等.塔中地区中-下奥陶统鹰山组沉积相及沉积模式[J].油气藏评价与开发, 2013, 3(1):1-8.LI Yingtao, BAI Xiaoliang, SU Bingrui, et al.Sedimentary facies and depositional model of middle-lower Ordovician Yingshan Formation in Tazhong area[J].Reservoir Evaluation and Development, 2013, 3(1):1-8.
[18] 马安来, 金之钧, 李慧莉, 等.塔里木盆地顺北地区奥陶系超深层油藏蚀变作用及保存[J].地球科学, 2020, 45(5):1737-1753.MA Anlai, JIN Zhijun, LI Huili, et al.Secondary alteration and preservation of ultra-deep Ordovician oil reservoirs of north Shuntuoguole area of Tarim Basin, NW China[J].Earth Science, 2020, 45(5):1737-1753.
[19] 程传捷, 于炳松, 武重阳, 等.塔里木盆地顺北地区奥陶系一间房组碳酸盐岩成岩相研究[J].石油实验地质, 2020, 42(1):42-52.CHENG Chuanjie, YU Bingsong, WU Chongyang, et al.Diagenetic facies of carbonate rocks in Yijianfang Formation, Shunbei area, Tarim Basin[J].Petroleum Geology&Experiment, 2020, 42(1):42-52.
[20] 韩强, 云露, 蒋华山, 等.塔里木盆地顺北地区奥陶系油气充注过程分析[J].吉林大学学报(地球科学版), 2021, 51(3):645-658.HAN Qiang, YUN Lu, JIANG Huashan, et al.Marine oil and gas filling and accumulation process in the north of Shuntuoguole area in northern Tarim Basin[J].Journal of Jilin University (Earth Science Edition), 2021, 51(3):645-658.
[21] 陈梦雪.塔里木顺北-顺南地区中下奥陶统沉积-层序演化研究[D].北京:中国石油大学(北京), 2018.CHEN Mengxue.A study on sedimentary sequence evolution of the Middle-Lower Ordovician in Shunbei-Shunnan area in Tarim[D].Beijing:China University of Petroleum (Beijing), 2018.
[22] 李兴旺.塔里木盆地顺北地区奥陶系碳酸盐岩储层特征研究[D].成都:成都理工大学, 2020.LI Xingwang.Sedimentary facies and depositional model of middlelower Ordovician Yingshan Formation in Tazhong area[D].Chengdu:Chengdu University of Technology, 2020.
[23] 尚凯, 吕海涛, 曹自成, 等.塔里木盆地顺托果勒低隆起一间房组分布及地质意义[J].石油实验地质, 2018, 40(3):353-361.SHANG Kai, LYU Haitao, CAO Zicheng, et al.Distribution and significance of Middle Ordovician Yijianfang Formation in Shuntuoguole lower uplift, Tarim Basin[J].Petroleum Geology&Experiment, 2018, 40(3):353-361.
[24] 赵晓辰, 刘池洋, 赵岩, 等.鄂尔多斯西南缘水泉岭组碳酸盐岩地球化学特征[J].西北大学学报(自然科学版), 2017, 47(1):101-109.ZHAO Xiaochen, LIU Chiyang, ZHAO Yan, et al.Geochemical characteristics of the Shuiquanling Formation carbonates in the southwestern margin of Ordos Basin[J].Journal of Northwest University (Natural Science Edition), 2017, 47(1):101-109.
[25] 吴朝东, 杨承运, 陈其英.湘西黑色岩系地球化学特征和成因意义[J].岩石矿物学杂志, 1999, 18(1):28-29.WU Chaodong, YANG Chengyun, CHEN Qiying.The origin and Geochemical characteristics of upper sinain lower Cambrian black shales in western Hunan[J].Acta Petrologica et Mineralogica, 1999, 18(1):28-29.
[26] VEIZER J, BUHL D, DIENER A, et al.Strontium isotope stratigraphy:Potential resolution and event correlation[J].Palaeogeography, Palaeoclimatology, Palaeoecology, 1997, 132(1):65-77.
[27] 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 the Upper Cambrian in zibo area, shandong[J].Geoscience, 2001, 15(4):377-382.
[28] 侯恩刚, 高金汉, 王训练, 等.西藏改则上三叠统日干配错组碳酸盐岩地球化学特征及沉积环境意义[J].矿物岩石地球化学通报, 2015, 34(3):556-563.HOU Engang, GAO Jinhan, WANG Xunlian, et al.Geochemical characteristics and environment significance of the Upper Triassic Riganmisuo Formation in Gize, Tibet[J].Bulletin of Mineralogy, Petrology and Geochemistry, 2015, 34(3):556-563.
[29] 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(01):4-9.KUANG Shaoping, XU Zhong, ZHANG Shusheng, et al.Applying geochemistry to research into Meso-Cenozoic climate:Discussion on Jurassic climatic change in Sichuan Basin, China[J].Journal of Qingdao University of Science and Technology (Natural Science Edition), 2002(1):4-9.
[30] 汪宗欣, 吕修祥, 钱文文.寒武系海相碳酸盐岩元素地球化学特征及其油气地质意义:以塔里木盆地柯坪地区肖尔布拉克组为例[J].天然气地球科学, 2017, 28(7):1085-1095.WANG Zongxin, LYU Xiuxiang, QIAN Wenwen.Geochemical characteristics of the Cambrian marine carbonate elements and its petroleum geological significance:Case study of Xiaoerbu-lake Formation in Keping area of Tairm Basin[J].Natural Gas Geoscience, 2017, 28(7):1085-1095.
[31] TYSON R V, PEARSON T H.Modern and ancient continental shelf anoxia:An overview[J].Arctic&Alpine Research, 1991, 59(1):1-24.
[32] JONES B, MANNING D A C.Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones[J].Chemical Geology, 1994, 111(1/2/3/4):111-129.
[33] 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.
[34] 高志勇, 白斌, 朱如凯, 等.大巴山与龙门山前晚三叠世构造运动的储集层沉积学响应[J].古地理学报, 2012, 14(6):801-812.GAO Zhiyong, BAI Bin, ZHU Rukai, et al.Reservior sedimentary response to tectonic movement of the Late Triassic in front of Dabashan and Longmen Mountains[J].Journal of Palaeogeography (Chinese Edition), 2012, 14(6):801-812.
[35] 曾允孚, 夏文杰.沉积岩石学[M].北京:地质出版社, 1986.ZENG Yunfu, XIA wenjie.Sedimentary petrology[M].Beijing:Geological Publishing House, 1986.
[36] 赖锦, 刘秉昌, 冯庆付, 等.鄂尔多斯盆地靖边气田马家沟组五段白云岩沉积微相测井识别与评价[J].地质学报, 2020, 94(5):1551-1567.LAI Jin, LIU Bingchang, FENG Qingfu, et al.Well logging identification and evaluation of depositional microfacies in dolostones from the 5th member of the Ordovician Majiagou Formation in the Jingbian gas field, Ordos Basin[J].Acta Geolo-gica Sinica, 2020, 94(5):1551-1567.
[37] 李多丽, 刘兴礼, 钟广法, 等.塔中Ⅰ号波折带礁滩型储集层沉积微相成像测井解释[J].新疆石油地质, 2009, 30(2):197-200.LI Duoli, LIU Xingli, ZHONG Guangfa, et al.Interpretation of imaging logs of sedimentary microfacies of reef-flat reservoir in Tazhong No.1 slope break zone, Tarim Basin[J].Xinjiang Petroleum Geology, 2009, 30(2):197-200.
[38] 朱玺.塔里木盆地中央隆起区鹰山组层序地层及沉积相研究[D].北京:中国地质大学(北京), 2014.ZHU Xi.Study on sequence stratigraphy and sedimentary facies of Yingshan Formation in central uplift area of Zhuxi Tarim Basin[D].Beijing:China University of Geosciences (Beijing), 2014.
[39] 曹康.塔里木盆地奥陶系中统一间房组沉积相研究[D].成都:西南石油大学, 2017.CAO Kang.Sedimentary facies of the Yijianfang Formation in the Ordovician of Tarim Basin[D].Chengdu:Southwest Petroleum University, 2017.
[1] 卜旭强, 王来源, 朱莲花, 黄诚, 朱秀香. 塔里木盆地顺北油气田奥陶系断控缝洞型储层特征及成藏模式[J]. 岩性油气藏, 2023, 35(3): 152-160.
[2] 杜江民, 刘泊远, 张毅, 贾志伟, 付基友, 龙鹏宇, 罗金洋, 盛军. 中国典型白云岩储集层特征及成藏模式[J]. 岩性油气藏, 2023, 35(3): 86-98.
[3] 宋兴国, 陈石, 杨明慧, 谢舟, 康鹏飞, 李婷, 陈九洲, 彭梓俊. 塔里木盆地富满油田FⅠ16断裂发育特征及其对油气分布的影响[J]. 岩性油气藏, 2023, 35(3): 99-109.
[4] 倪新锋, 沈安江, 乔占峰, 郑剑锋, 郑兴平, 杨钊. 塔里木盆地奥陶系缝洞型碳酸盐岩岩溶储层成因及勘探启示[J]. 岩性油气藏, 2023, 35(2): 144-158.
[5] 陈中红, 柴智. 原油混合后成熟度参数的差异性及其地质意义——以塔北隆起托甫台地区奥陶系为例[J]. 岩性油气藏, 2022, 34(5): 38-49.
[6] 张凤奇, 李宜浓, 罗菊兰, 任小锋, 张兰馨, 张芥瑜. 鄂尔多斯盆地西部奥陶系乌拉力克组页岩微观孔隙结构特征[J]. 岩性油气藏, 2022, 34(5): 50-62.
[7] 张俊龙, 何幼斌, 梁建设, 邱春光, 吴东胜, 李华, 童乐. 东非海岸盆地下侏罗统沉积特征及其控源作用[J]. 岩性油气藏, 2022, 34(4): 128-140.
[8] 宋传真, 马翠玉. 塔河油田奥陶系缝洞型油藏油水流动规律[J]. 岩性油气藏, 2022, 34(4): 150-158.
[9] 陈袁, 廖发明, 吕波, 贾伟, 宋秋强, 吴燕, 亢鞠, 鲜让之. 塔里木盆地迪那2气田古近系离散裂缝表征与建模[J]. 岩性油气藏, 2022, 34(3): 104-116.
[10] 邱晨, 闫建平, 钟光海, 李志鹏, 范存辉, 张悦, 胡钦红, 黄毅. 四川盆地泸州地区奥陶系五峰组—志留系龙马溪组页岩沉积微相划分及测井识别[J]. 岩性油气藏, 2022, 34(3): 117-130.
[11] 罗振锋, 苏中堂, 廖慧鸿, 黄文明, 马慧, 佘伟. 鄂尔多斯盆地中东部米脂地区奥陶系马五5亚段叠层石白云岩特征及其地质意义[J]. 岩性油气藏, 2022, 34(2): 86-94.
[12] 张梦琳, 李郭琴, 何嘉, 衡德. 川西南缘天宫堂构造奥陶系五峰组—志留系龙马溪组页岩气富集主控因素[J]. 岩性油气藏, 2022, 34(2): 141-151.
[13] 屈童, 高岗, 徐新德, 王瑞, 甘军, 梁刚, 游君君. 三角洲—浅海沉积体系泥质沉积规律模拟实验——以琼东南盆地崖南凹陷为例[J]. 岩性油气藏, 2022, 34(1): 24-33.
[14] 王素英, 张翔, 田景春, 彭明鸿, 郑潇宇, 夏永涛. 塔里木盆地顺北地区柯坪塔格组沉积演化及沉积分异模式[J]. 岩性油气藏, 2021, 33(5): 81-94.
[15] 叶涛, 王清斌, 代黎明, 陈容涛, 崔普媛. 台地相碳酸盐岩层序划分新方法——以渤中凹陷奥陶系为例[J]. 岩性油气藏, 2021, 33(3): 95-103.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] 黄思静,黄培培,王庆东,刘昊年,吴　萌,邹明亮. 胶结作用在深埋藏砂岩孔隙保存中的意义[J]. 岩性油气藏, 2007, 19(3): 7 -13 .
[2] 刘震, 陈艳鹏, 赵阳,, 郝奇, 许晓明, 常迈. 陆相断陷盆地油气藏形成控制因素及分布规律概述[J]. 岩性油气藏, 2007, 19(2): 121 -127 .
[3] 丁超，郭兰，闫继福. 子长油田安定地区延长组长6 油层成藏条件分析[J]. 岩性油气藏, 2009, 21(1): 46 -50 .
[4] 李彦山，张占松，张超谟，陈鹏. 应用压汞资料对长庆地区长6 段储层进行分类研究[J]. 岩性油气藏, 2009, 21(2): 91 -93 .
[5] 罗 鹏,李国蓉,施泽进,周大志,汤鸿伟,张德明. 川东南地区茅口组层序地层及沉积相浅析[J]. 岩性油气藏, 2010, 22(2): 74 -78 .
[6] 左国平，屠小龙，夏九峰. 苏北探区火山岩油气藏类型研究[J]. 岩性油气藏, 2012, 24(2): 37 -41 .
[7] 邢二涛，张云锋. 水平井开发技术在贝中区N1 段应用研究[J]. 岩性油气藏, 2010, 22(Z1): 93 -95 .
[8] 王飞宇. 提高热采水平井动用程度的方法与应用[J]. 岩性油气藏, 2010, 22(Z1): 100 -103 .
[9] 袁云峰，才业，樊佐春，姜懿洋，秦启荣，蒋庆平. 准噶尔盆地红车断裂带石炭系火山岩储层裂缝特征[J]. 岩性油气藏, 2011, 23(1): 47 -51 .
[10] 袁剑英，付锁堂，曹正林，阎存凤，张水昌，马达德. 柴达木盆地高原复合油气系统多源生烃和复式成藏[J]. 岩性油气藏, 2011, 23(3): 7 -14 .

陇ICP备17006252号
版权所有© 2018 中国石油集团西北地质研究所有限公司《岩性油气藏》编辑部

地址：甘肃省兰州市城关区雁儿湾路535号(陇ICP备17006252号)    电话：0931-8686158;8686058;8686288    邮箱：yxyqc@petrochina.com.cn

甘公网安备 62010202002827号

本系统由北京玛格泰克科技发展有限公司设计开发