天然气地球科学
高级检索
作者投稿 专家审稿 编辑办公

天然气地球科学

• 天然气地球化学 • 上一篇    下一篇

延吉盆地铜佛寺组烃源岩地球化学特征及勘探潜力评价

袁近洋，朱建伟，林波，董清水，钟延秋，王世辉   

  1. 1.吉林大学地球科学学院，吉林 长春13006;2.吉林省油页岩与共生能源矿产重点实验室，长春 中国 13006;
    3.大庆油田有限责任公司勘探开发研究院，黑龙江 大庆 163712
  • 收稿日期:2014-02-03 修回日期:2014-03-31 出版日期:2015-01-10 发布日期:2015-01-10
  • 通讯作者: 朱建伟(1961-)，男，辽宁法库人，教授，主要从事油气勘探和油气田开发、地震地质的教学和研究. E-mail:hujw@jlu.edu.cn.
  • 作者简介:袁近洋(1988-)，男，四川南充人，硕士研究生，主要从事油气勘探和油气田开发研究. E-mail:yuanjy_jlu@163.com.
  • 基金资助:

    全国油气资源战略选区调查与评价国家专项(第二批)(编号:2009GYXQ12-04)资助.

Source Rocks Geochemical Characteristic and Exploration Potential Evaluation of Tongfosi Formation in Yanji Basin

YUAN Jin-yang，ZHU Jian-wei，LIN Bo，DONG Qing-shui，ZHONG Yan-qiu，WANG Shi-hui   

  1. 1.College of Earth Sciences,Jilin University,Changchun 130061,China;
    2.Key Laboratory for Oil Shale and Coexistent Energy Minierals of Jilin Province,Changchun 130061,China;
    3.Exploration and Development Research Institute of Daqing Oilfield Company Ltd,Daqing 163712,China
  • Received:2014-02-03 Revised:2014-03-31 Online:2015-01-10 Published:2015-01-10

PDF (PC)

525

摘要：

延吉盆地为中生代断陷盆地。根据20口岩心及测井资料分析，延吉盆地铜佛寺组主要发育扇三角洲相和湖泊相2种沉积相类型，暗色泥岩厚度达20~500m。基于对700余块铜佛寺组暗色泥岩样品的有机碳、氯仿沥青“A”、生烃潜量、有机质类型的测试数据，确定出铜佛寺组一段、二段、三段都发育有较高有机质丰度的烃源岩，有机质类型以Ⅱ型为主。90块暗色泥岩的RO值测试数据表明，铜佛寺组暗色泥岩除德新凹陷铜佛寺组三段部分样品未达到生油门限外，其余都处于开始生烃的低熟—成熟阶段。综合各种测试分析数据，认为延吉盆地除了德新凹陷铜佛寺组三段为低熟烃源岩之外，铜佛寺组暗色泥岩均为成熟良好的有效烃源岩。综合烃源岩特征及有效烃源岩分布等，认为延吉盆地具有良好的油气资源潜力，并依据油气显示(产量)、沉积相、圈闭类型等5个评价参数，优选出延吉盆地Y13井—Y20井区、延10井—延12井区、Y1井—Y3井区为勘探开发有利区。

关键词: 延吉盆地, 铜佛寺组, 烃源岩, 地球化学特征, 勘探开发有利区

Abstract:

The Yanji Basin is a Mesozoic fault basin.Based on cores and well logs of 20 boreholes,facies of the Tongfosi Formation are mainly fan-delta and lacustrine.Thickness of dark-colored mudstone ranges from 20 to 500m.Analyses of organic carbon,chloroform bitumen “A”,hydrocarbon generation potential,and organic matter type on more than 700 dark-colored mudstone samples show that,source rocks of the First,Second,and Third members of the Tongfosi Formation have relatively high organic matter concentration and are characterized by type-Ⅱ kerogen.Results of organic maturity degree（RO）analysis on 90 dark-colored mudstone samples show that,apart from part of the third member in the Dexin Sag,most of the dark-colored mudstone of the Tongfosi Formation in the Yanji Basin is slightly mature or mature,and is interpreted as effective source rock.Thus,the Yanji Basin is a potentially productive petroliferous basin.Based on five evaluation indices,such as hydrocarbon production,facies,and trap types,a series of well blocks(i.e.,Y 13 to Y 20,Yan 10 to Yan 12,and Y 1 to Y 3) are selected as priority prospects.

 

Key words: Yanji Basin, Tongfosi Formation, Source rocks, Geochemical characteristic, Exploration and development target regions

中图分类号: 

  • P618.13

［1］Yao Xinmin,Zhou Zhixiang,Pei Junyue.Inquisition of petroleum geological feature of Yanji Basin[J].Oil and Gas Geology,1991,12(4):464-470.［姚新民,周志祥,裴军跃.延吉盆地石油地质特征初探[J].石油与天然气地质,1991,12(4):464-470.］
［2］Xu Yan,Liu Li,Zhao Yujun.The oil system and exploration perspective in Yanji Basin[J].Journal of Jilin University:Earth Science Edition,2004,34(2):227-230,241.［许岩,刘立,赵羽君.延吉盆地含油气系统与勘探前景[J].吉林大学学报:地球科学版,2004,34(2):227-230,241.］
［3］Wang Xianmei.Sedimentary Sequence Study about Cretaceous Strata in Yanji Basin［D］.Daqing:Daqing Petroleum Institute,2003:22-35.［王先美.延吉盆地白垩纪地层充填序列研究［D］.大庆:大庆石油学院,2003:22-35.］
［4］Shi Chunlei.Cretaceous Strata Sequence and Basin Evolution of Yanji Basin［D］.Changchun:Jilin University,2008:7-31.［石春磊.延吉盆地白垩纪地层序列及盆地演化［D］.长春:吉林大学,2008:7-31.］
［5］Cui Tongcui,Zhang Ying,Zhang Yanxin.Strata sequence of Late Mesozioc in Yanji Basin[J].Petroleum Geology & Oilfield Development in Daqing,1994,13(2):25-28.［崔同翠,张莹,张艳芯.对延吉盆地晚中生代地层层序的认识[J].大庆石油地质与开发,1994,13(2):25-28.］
［6］Feng Changshou.The sedimentation and oil-gas characteristics of the Lower Cretaceous,Tongfosi Formation and Dalazi Formation,Yanji Basin[J].Jilin Geology,2002,21(3):33-40.［冯昌寿.延吉盆地下白垩统铜佛寺组-大砬子组沉积与油气特征[J].吉林地质,2002,21(3):33-40.］
［7］Zhao Gang.Research on Characteristics of Sedimentary Facies and Hydrocarbon Accumulation in Tongfosi and Dalazi Formation of Yanji Basin［D］.Changchun:Jilin University,2012:12-16.［赵刚.延吉盆地铜佛寺组和大砬子组沉积相及油气成藏特征研究［D］.长春:吉林大学,2012:12-16.］
［8］Tenger,Gao Changlin,Hu Kai,et al.High quality source rocks of lower combination in the northern Upper-Yangtze area and their hydrocarbon potential[J].Natural Gas Geoscience,2007,18(2):254-259.［腾格尔,高长林,胡凯,等.上扬子北缘下组合优质烃源岩分布及生烃潜力评价[J].天然气地球科学,2007,18(2):254-259.］
［9］Qing Jianzhong,Liu Baoquan,Guo Jianying,et al.Discussion on the evaluation standards of carbonate source rocks[J].Petroleum Geology & Experiment,2004,26(3):281-286.［秦建中,刘宝泉,国建英,等.关于碳酸盐烃源岩的评价标准[J].石油实验地质,2004,26(3):281-286.］
［10］Wang Jie,Chen Jianfa,Dou Qilong.Evaluation of the hydrocarbon-generating potential for the possible hydrocarbon source rocks of the Middle-Upper Proterozoic in north Huabei area[J].Petroleum Geology & Experiment,2004,26(2):206-211.［王杰,陈践发,窦启龙.华北北部中、上元古界生烃潜力特征研究[J].石油实验地质,2004,26(2):206-211.］
［11］Hu Jianyi,Huang Dipan,Xu Shubao,et al.The Bases of Nonmarine Petroleum Geology in China［M］.Beijing:Petroleum Industry Press,1991:181-186.［胡见义,黄第藩,徐树宝,等.中国陆相石油地质理论基础［M］.北京:石油工业出版社,1991:181-186.］
［12］China National Petroleum Corporation.Continental Source Rocks Geochemical Evaluation Methods［S］.Beijing:Petroleum Industry Press,1995:3-8.［中国石油天然气总公司.陆相烃源岩地球化学评价方法［S］.北京:石油工业出版社,1995:3-8.］
［13］Wang Zhensheng,Liu Qingxin,Tan Zhenhua,et al.Comprehensive evaluation of source rock of Qinan Sag,Huanghua Depression[J].Natural Gas Geoscience,2009,20(6):968-971.［王振升,刘庆新,谭振华,等.黄骅坳陷歧南凹陷烃源岩评价[J].天然气地球科学,2009,20(6):968-971.］
［14］Zhang Houfu,Fang Chaoliang,Gao Xianzhi,et al.Petroleum Geology［M］.Beijing:Petroleum Industry Press,2007:83-100.［张厚福,方朝亮,高先志,等.石油地质学［M］.北京:石油工业出版社,2007:83-100.］
［15］Lu Shuangfang,Zhang Min.Petroleum Geochemistry［M］.Beijing:Petroleum  Industry  Press,2008:201-226.［卢双舫,张敏.油气地球化学［M］.北京:石油工业出版社,2008:201-226.］
［16］Cheng Dingsheng.Review of source rock maturity evalution by organic petrology method[J].Xinjiang Petroleum Geology,1998,19(5):428-432.［程顶胜.烃源岩有机质成熟度评价方法综述[J].新疆石油地质,1998,19(5):428-432.］
［17］Chen Yicai,Shen Zhongmin,Luo Xiaoping.Petroleum and Natural Gas Geochemistry［M］.Beijing:Petroleum Industry Press,2007:190-195.［陈义才,沈忠民,罗小平.石油与天然气有机地球化学［M］.北京:石油工业出版社,2007:190-195.］
［18］Li Xiangchen.Study on effective hydrocarbon source rocks and relationship between them andnatural gas reservoirs[J].Natural Gas Geoscience,2003,14(1):53-56.［李祥臣.有效烃源岩及其与天然气藏关系探讨[J].天然气地球科学,2003,14(1):53-56.］
［19］Rao Dan,Zhang Pinglan,Qiu Yunyu.Discussion  on lower limit of content of organic matters for effective source rocks[J].Petroleum Geology & Experiment,2003,25(supplement):578-581.［饶丹,章平澜,邱蕴玉.有效烃源岩下限指标初探[J].石油实验地质,2003,25(增刊):578-581.］
［20］Zhu Guangyou,Jin Qiang,Zhang Shuichang,et al.Combination characteristics of lake facies source rock in the Shahejie Formation,Dongying Depression[J].Acta Geologica Sinica,2004,78(3):416-427.［朱光有,金强,张水昌,等.东营凹陷沙河街组湖相烃源岩的组合特征[J].地质学报,2004,78(3):416-427.］
［21］Qin Jianzhong.Rource Rock in China［M］.Beijing:Science Press,2007:10-20.［秦建中.中国烃源岩［M］.北京:科学出版社,2007:10-20.］
［22］Zhu Jianwei,Wang Fei,Zhao Gang,et al.Sedimentary facies and reservoir characteristics of Dalazi Formation in Yanji Basin[J].Journal of Jilin University:Earth Science Edition,2012,42(supplement 2):1-10.［朱建伟,王菲,赵刚,等.延吉盆地大砬子组沉积相及储层特征[J].吉林大学学报:地球科学版,2012,42(增刊2):1-10.］
[1] 傅宁,刘建升. 北部湾盆地流二段3类烃源岩的生烃成藏特征[J]. 天然气地球科学, 2018, 29(7): 932-941.
[2] 贾智彬,侯读杰,孙德强,姜玉涵,张自鸣,洪梅. 贵州地区牛蹄塘组底部烃源岩地球化学特征[J]. 天然气地球科学, 2018, 29(7): 1031-1041.
[3] 陈斐然，张义杰，朱光有，张宝收，卢玉红，张志遥. 塔里木盆地台盆区深层天然气地球化学特征及成藏演化[J]. 天然气地球科学, 2018, 29(6): 880-891.
[4] 邓焱，胡国艺，赵长毅. 四川盆地龙岗气田长兴组—飞仙关组天然气地球化学特征及成因[J]. 天然气地球科学, 2018, 29(6): 892-907.
[5] 程志强，王飞宇，师玉雷，冯伟平，谢佩宇，任利兵，吴子强,江涛，赵志刚. 二连盆地乌里雅斯太凹陷南洼烃源岩有机相与生烃特征[J]. 天然气地球科学, 2018, 29(5): 696-707.
[6] 申宝剑，秦建中，腾格尔，潘安阳，仰云峰，边立曾. 中国南方海相烃源岩中细菌状化石识别[J]. 天然气地球科学, 2018, 29(4): 510-517.
[7] 贺领兄，宋维刚，安生婷，徐永锋，沈娟，路超，王军. 青海东昆仑地区八宝山盆地烃源岩有机地球化学特征与页岩气勘探前景[J]. 天然气地球科学, 2018, 29(4): 538-549.
[8] 邢 舟,曹高社，毕景豪，周新桂,张交东. 南华北盆地禹州地区ZK0606钻孔上古生界煤系烃源岩评价[J]. 天然气地球科学, 2018, 29(4): 518-528.
[9] 杨飞，蒲秀刚，姜文亚，韩文中，张伟，时战楠，林常梅. 渤海湾盆地沧东凹陷孔二段细粒相区有机地球化学特征[J]. 天然气地球科学, 2018, 29(4): 550-558.
[10] 白雪峰, 梁江平, 张文婧, 付丽, 彭建亮, 薛涛, 杨立伟, 刘继莹. 松辽盆地北部深层天然气地质条件、资源潜力及勘探方向[J]. 天然气地球科学, 2018, 29(10): 1443-1454.
[11] 秦胜飞，罗平，王铜山，王蓝军，马奎. 华北南缘东部新元古界冰碛砾岩层系中优质烃源岩的发现及地质意义[J]. 天然气地球科学, 2018, 29(1): 55-61.
[12] 李玉婷，黄志龙，安成龙，马强，王瑞，辛铭. 三塘湖盆地石炭系哈尔加乌组上、下段烃源岩特征及差异[J]. 天然气地球科学, 2018, 29(1): 73-86.
[13] 陈晓艳，田福清,邹华耀，郭柳汐,芦晓伟，殷杰，王道军. 湖相烃源岩热演化生烃研究——基于冀中坳陷烃源岩加水热模拟实验[J]. 天然气地球科学, 2018, 29(1): 103-113.
[14] 王钊，周新平，李树同，李士祥,邱军利，张文选,王琪. 鄂尔多斯盆地吴起地区长9段和长10段原油地球化学特征对比[J]. 天然气地球科学, 2017, 28(9): 1385-1395.
[15] 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.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!