高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

鄂尔多斯盆地延长组湖相黏土岩分类和沉积环境探讨

刘群 袁选俊 林森虎 王岚 郭浩 潘松圻 姚泾利

刘群, 袁选俊, 林森虎, 王岚, 郭浩, 潘松圻, 姚泾利. 鄂尔多斯盆地延长组湖相黏土岩分类和沉积环境探讨[J]. 沉积学报, 2014, 32(6): 1016-1025.
引用本文: 刘群, 袁选俊, 林森虎, 王岚, 郭浩, 潘松圻, 姚泾利. 鄂尔多斯盆地延长组湖相黏土岩分类和沉积环境探讨[J]. 沉积学报, 2014, 32(6): 1016-1025.
LIU Qun, YUAN Xuan-jun, LIN Sen-hu, WANG Lan, GUO Hao, PAN Song-qi, YAO Jing-li. The Classification of Lacustrine Mudrock and Research on Its' Depositional Environment[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1016-1025.
Citation: LIU Qun, YUAN Xuan-jun, LIN Sen-hu, WANG Lan, GUO Hao, PAN Song-qi, YAO Jing-li. The Classification of Lacustrine Mudrock and Research on Its' Depositional Environment[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1016-1025.

鄂尔多斯盆地延长组湖相黏土岩分类和沉积环境探讨

基金项目: 国家油气重大专项“岩性地层油气藏成藏规律、关键技术及目标评价”(编号:2011ZX05001)资助
详细信息
    作者简介:

    刘群 女 1991年出生 硕士研究生 湖盆沉积学与非常规石油地质 E-mail:ro1ql14@abdn.ac.uk

  • 中图分类号: TE121.3+1

The Classification of Lacustrine Mudrock and Research on Its' Depositional Environment

  • 摘要: 鄂尔多斯盆地三叠系延长组长7油层组沉积了区域分布的大套湖相黏土岩,它不但是鄂尔多斯盆地中生界最重要的烃源岩,同时也是目前致密油/页岩油勘探的主要领域.作者在对国内外黏土岩分类及其成因机制等系统调研基础上,通过对工区25口连续取芯井的岩芯描述和400余块典型黏土岩薄片观察,并充分应用X衍射、有机地球化学等分析测试资料,提出了湖相黏土岩的分类方案与基本特征,探讨了不同类型黏土岩形成的沉积环境.根据岩石组分、沉积构造等特征,鄂尔多斯盆地延长组长7油层组黏土岩主要发育5种类型:①块状泥岩;②粒序层理泥岩;③波状纹层页岩;④平直纹层页岩;⑤似块状页岩.该成因分类方案将黏土岩类型与沉积环境相结合.指出受三角洲前缘影响的浅湖区以块状泥岩为主;受湖流和波浪影响的浅湖—半深湖环境以波状纹层页岩为主;深湖静水区以平直纹层状页岩为主;深湖坳陷区以粒序层理泥岩为主;火山灰爆发时期以似块状页岩为主.粒序层理泥岩是致密油赋存的主要类型,有机碳平均含量为6%;似块状页岩是页岩油赋存的主要类型,有机碳平均含量为17.17%.
  • [1] Macquaker J H S, Adams A E. Macquaker J H S, Adams A E. Maximizing information from fine-grained sedimentary rocks: an inclusive nomenclature for mudstones [J]. Journal of Sedimentary Research, 2003, 73(5): 735-744
    [2] П.П.阿弗杜辛. 粘土沉积岩[M]. 周鸿生,译. 北京:地质出版社,1956:7-8[П.П.阿弗杜辛. Claystone[M]. Translated by Zhou Hongsheng. Beijing: Geological Publishing House, 1956: 7-8]
    [3] Л.Б.鲁欣. 沉积岩石学手册(下册)[M]. 北京:中国工业出版社,1964:101-106[Л.Б.Rusy. Sedimentary Rocks [M]. Beijing: China Architecture & Building Press, 1964: 101-106]
    [4] 方邺森,任磊夫. 沉积岩石学教程[M]. 北京:地质出版社,1987:139-140[Fang Yesen, Ren Leifu. Sedimentology[M]. Beijing: Geological Publishing House, 1987: 139-140]
    [5] H·布拉特,G·V·米德顿,R·C·穆雷. 沉积岩成因[M]. 北京:科学出版社,1978:266-284[H·Blatt, G·V·Middleton, R·C·Millon. The Attributes of Sedimentary Rocks [M]. Beijing: Science Press, 1978: 266-284]
    [6] 冯增昭,等. 沉积岩石学(上册)[M]. 北京:石油工业出版社,1994:124-125[Feng Zengzhao, et al. Sedimentology [M]. Beijing: Petroleum Industry Press, 1994: 124-125]
    [7] Josef P. Werne, et al. An integrated assessment of a “type euxinic”deposit: evidence for multiple controls on black shale deposition in the middle Devonian Oatka Creek Formation[J]. American Journal of Science, 2002, 302(2): 110-143
    [8] Ghadeer S G, Macquaker J H S. Sediment transport processes in an ancient mud-dominated succession: a comparison of processes operating in marine offshore settings and anoxic basinal environments[J]. Journal of the Geological Society of London, 2011, 168(5): 1121-1132
    [9] Guy P A. Mud dispersal across a Cretaceous prodelta: Storm-generated, wave-enhanced sediment gravity flows inferred from mudstone microtexture and microfacies[J]. Sedimentology, 2014, 61(3): 609-647
    [10] Guy P A, Macquaker J H S, Varban B L, Bedload transport of mud across a wide, storm influenced ramp: Cenomanian-Turonian Kaskapau Formation, western Canada Foreland Basin[J]. Journal of Sedimentary Research, 2012, 82(11): 801-822
    [11] Mulder T, Syvitski J P M. Turbidity currents generated at river mouths during exceptional discharges to the world oceans[J]. Journal of Geology, 1995, 103: 285-299
    [12] Mulder T, Migeon S, Savoye B, et al. Inversely graded turbidite sequences in the deep Mediterranean: a record of deposits from flood generated turbidity currents? [J]. Geo-Marine Letters, 2001, 21(2): 86-93
    [13] 李万春,李世杰,濮培民. 高分辨率古环境指示器—湖泊纹泥研究综述[J]. 地球科学进展,1999,14(2):172-176 [Li Wanchun, Li Shijie, Pu Peimin. Review on the high-resolution varved lake sediments as a proxy of paleoenvironment[J]. Advance in Earth Sciences, 1999, 14(2): 172-176]
    [14] 邓宏文,钱凯. 深湖相泥岩的成因类型和组合演化[J]. 沉积学报,1990,8(3):1-21 [Deng Hongwen, Qian Kai. The genetic types and association evolution of deep lacustrine facies mudstone[J]. Acta Sedimentologica Sinica, 1990, 8(3): 1-21]
    [15] 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,2002:36-37[Yang Junjie. On Structural Evolution and Hydrocarbon Distribution in Ordos Basin [M]. Beijing: Petroleum Industry Press, 2002: 36-37]
    [16] Zhao M, Behr H, Ahrendt H, et al. Thermal and tectonic history of the Ordos Basin, China: Evidence from apatite fission track analysis, vitrinite reflectance, and K-Ar dating[J]. AAPG Bulletin, 1996, 80(7): 1110-1134
    [17] Wang B, Al-Aasm I S. Karst-controlled diagenesis and reservoir development; example from the Ordovician main reservoir carbonate rocks on the eastern margin of the Ordos Basin, China[J]. AAPG Bulletin, 2002, 86(9): 1639-1658
    [18] 林森虎. 鄂尔多斯盆地长7段细粒沉积物特征与致密油分布[D]. 北京:中国石油勘探开发研究院,2012:1-106[Lin Senhu. The characteristics of fine-grained sedimentary rocks and tight oil distribution in Chang7 member, Ordos Basin [D]. Beijing: Research Institute of China Exploration and Development, 2012: 1-106]
    [19] 王冠民. 济阳坳陷古近系页岩的纹层组合及成因分类[J]. 吉林大学科学学报:地球科学版,2012,42(3): 666-671,680[Wang Guanmin. Laminae combination and genetic classification of Eogene shale in Jiyang depression[J]. Journal of Jilin University: Earth Science Edition, 2012, 42(3): 666-671, 680]
    [20] 刘招君,孟庆涛,柳蓉. 中国陆相油页岩特征及成因类型[J]. 古地理学报,2009,11(1):105-114[Liu Zhaojun, Meng Qingtao, Liu Rong. Characteristics and genetic types of continental oil shales in China[J]. Journal of Palaeogeography, 2009, 11(1): 105-114]
    [21] 郭巍,刘招君,宋玉勤,等. 青海一甘肃民和盆地油页岩的成因类型及特征[J]. 地质通报,2009,28(6):780-786[Guo Wei, Liu Zhaojun, Song Yuqin, et al. Genetic type and features of oil shale in the Minhe Basin, Qinghai-Gansu provinces, China [J]. Geological Bulletin of China, 2009, 28 (6): 780-786]
    [22] 姜在兴,梁超,吴靖,等. 含油气细粒沉积岩研究的几个问题[J]. 石油学报,2013,34(6):1031-1039[Jiang Zaixing, Liang Chao, Wu Jing, et al. Several issues in sedimentological studies on hydrocarbon-bearing fine-grained sedimentary rocks[J]. Acta Petrolei Sinica, 2013, 34(6): 1031-1039]
    [23] 张文正,杨华,彭平安,等. 晚三叠世火山活动对鄂尔多斯盆地长7优质烃源岩发育的影响[J]. 地球化学,2009,38(6):573-582[Zhang Wenzheng, Yang Hua, Peng Ping'an, et al. The influence of Late Triassic volcanism on the development of Chang 7 high grade hydrocarbon source rock in Ordos Basin[J]. Geochimica, 2009, 38(6): 573-582]
    [24] Bradley B. Sagemana. A tale of shales: the relative roles of production, decomposition, and dilution in the accumulation of organic-rich strata, Middle-Upper Devonian, Appalachian basin[J]. Chemical Geology, 2002, 95 (2003): 229-273
    [25] Demaison G J, Moore G T. Anoxic environments and oil source bed genesis[J]. AAPG Bulletin, 1980, 2(1): 9-31
    [26] Tyson R V. Sedimentation rate, dilution, preservation and total organic carbon: some results of a modeling study[J]. Organic Geochemistry, 2001, 32(2): 333-339
    [27] Stow D A V, Huc A Y & Bertrand. Depositional processes of black shales in deep water[J]. Marine and Petroleum Geology, 2001, 18(4): 491-498
    [28] Middleton G V, Hampton M A. Sediment Gravity Flow: Mechanics of Flow and Deposition[C]//Middleton G V, Bouma A H. Turbidites and Deep Water Sedimentation. Anaheim: SEPM pacific sec. short Course Note, 1973: 1-38
    [29] Yu Saitoh, Fujio Masuda. Spatial change of grading pattern of subaqueous flood deposits in lake Shinji, Japan[J]. Journal of Sedimentary Research, 2013, 83(2): 221-233
    [30] Mulder T, Alexander J. The physical character of subaqueous sedimentary density flows and their deposits[J]. Sedimentology, 2001, 48(2): 269-299
    [31] Mulder T, Migeon S, Savoye B, Faugeres J C. Reply to discussion by Shanmugam on Mulder et al. (2001, Geo-Marine Letters 21: 86-93) Inversely graded turbidite sequences in the deep Mediterranean. A record of deposits from flood generated turbidity currents? [J]. Geo-Marine Letters, 2002, 22(2): 112-120
    [32] Mulder T, Syvitski J P M, Migeon S, et al. Marine hyperpycnal flows; initiation, behavior and related deposits; a review [J]. Marine and Petroleum Geology, 2003, 20(6): 861-882
    [33] Schieber J. Reverse engineering mother nature—shale sedimentology from an experimental perspective. [J]. Sedimentology, 2011, 238(1): 1-22
    [34] Macquaker J H S, et al. Wave-enhanced sediment gravity flows and mud dispersal across continental shelves: Reappraising sediment transport processes operating in ancient mudstone successions[J]. Geology, 2010, 38(10): 947-950
    [35] Schieber J. Lenticular shale fabrics resulting from intermittent erosion of water-rich muds—Interpreting the rock record in the light of recent flume experiments[J]. Journal of Sedimentary Research, 2010, 80(1): 119-128
    [36] 王冠民,钟建华. 湖泊纹层的沉积机理研究评述与展望[J]. 岩石矿物学杂志,2004,23(1):43-48[Wang Guanming, Zhong Jianhua. A review and the prospects of the researches on sedimentary mechanism of lacustrine laminae[J]. Acta Petrologica et Mineralogica, 2004, 23(1): 43-48]
    [37] 刘传联,徐金鲤,汪品先. 藻类勃发——湖相油源岩形成的一种重要机制[J]. 地质论评,2001,47(2):207-210[Liu Chuanlian, Xu Jinli, Wang Pinxian. Algal blooms: the primary mechanism in the formation of lacustrine petroleum source rocks[J]. Geological Review, 2001, 47(2): 207-210]
    [38] Macquaker J H S, Keller M A, Davies S J. Algal blooms and marine snow: mechanisms that enhance preservation of organic carbon in ancient fine-grained sediments[J]. Journal of Sedimentary Research, 2010, 80(11): 934-942
  • [1] 尹泽, 刘自亮, 彭楠, 沈芳, 谭梦琪, 王玉冲, 梁雨晨, 王红伟.  鄂尔多斯盆地西缘上三叠统延长组沉积相特征研究 . 沉积学报, 2019, 37(1): 163-176. doi: 10.14027/j.issn.1000-0550.2018.156
    [2] 屈雪峰, 温德顺, 张龙, 崔争锋, 张瀚丹, 马静.  鄂尔多斯盆地延长组超低渗透油藏形成过程分析——以古峰庄-麻黄山地区为例 . 沉积学报, 2017, 35(2): 383-392. doi: 10.14027/j.cnki.cjxb.2017.02.015
    [3] 郑庆华, 柳益群.  鄂尔多斯盆地镇北地区延长组长4+5致密油层成岩作用及成岩相 . 沉积学报, 2015, 33(5): 1000-1012. doi: 10.14027/j.cnki.cjxb.2015.05.016
    [4] 明晓冉, 刘立, 刘娜娜, 宋土顺, 王福刚, 于严龙.  鄂尔多斯盆地JX井延长组砂岩固碳潜力分析 . 沉积学报, 2015, 33(1): 202-210. doi: 10.14027/j.cnki.cjxb.2015.01.021
    [5] 杨仁超, 金之钧, 孙冬胜, 樊爱萍.  鄂尔多斯晚三叠世湖盆异重流沉积新发现 . 沉积学报, 2015, 33(1): 10-20. doi: 10.14027/j.cnki.cjxb.2015.01.002
    [6] 鄂尔多斯盆地东北部上古生界煤系烃源岩17α(H)-重排藿烷类的分布及成因探讨 . 沉积学报, 2014, 32(4): 790-796.
    [7] 深水块状砂岩碎屑流成因的直接证据:“泥包砾”结构——以鄂尔多斯盆地上三叠统延长组研究为例 . 沉积学报, 2014, 32(4): 611-622.
    [8] 鄂尔多斯盆地延长组深水岩相发育特征及其石油地质意义 . 沉积学报, 2013, 31(05): 928-938.
    [9] 鄂尔多斯盆地余兴庄—子洲地区上古生界山3 2储层砂岩成岩作用与成岩相 . 沉积学报, 2011, 29(6): 1031-1040.
    [10] 鄂尔多斯盆地延长组长10期沉积环境与沉积体系 . 沉积学报, 2011, 29(6): 1105-1114.
    [11] 付锁堂.  晚三叠世鄂尔多斯盆地湖盆沉积中心厚层砂体特征及形成机制分析 . 沉积学报, 2010, 28(6): 1081-1089. doi: 
    [12] 马 强.  鄂尔多斯盆地伊陕斜坡中部长6油层组沉积微相及其含油性研究 . 沉积学报, 2009, 27(3): 443-451. doi: 
    [13] 赵俊兴.  鄂尔多斯盆地南部延长组长6时期物源状况分析 . 沉积学报, 2008, 26(4): 610-616. doi: 
    [14] 郭彦如 刘化清 李相博 完颜容 郑希民.  大型坳陷湖盆层序地层格架的研究方法体系 ———以鄂尔多斯盆地中生界延长组为例 . 沉积学报, 2008, 26(3): 384-391. doi: 
    [15] 李元昊.  鄂尔多斯盆地三叠系延长组震积岩特征研究 . 沉积学报, 2008, 26(5): 772-779. doi: 
    [16] 罗 忠.  层序界面对砂岩成岩作用及储层质量的影响——以鄂尔多斯盆地延河露头上三叠统延长组为例 . 沉积学报, 2007, 25(6): 903-914. doi: 
    [17] 吉利明.  陇东三叠系延长组主要油源岩发育时期的古气候特征 . 沉积学报, 2006, 24(3): 426-431. doi: 
    [18] 鄂尔多斯盆地陇东地区延长组沉积相特征与层序地层分析 . 沉积学报, 2006, 24(4): 549-554.
    [19] 侯方浩, 方少仙, 董兆雄, 赵敬松, 卢蜀秀, 吴诒, 陈娅娜.  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 . 沉积学报, 2003, 21(1): 106-112.
    [20] 高山林, 陈海泓, 窦伟坦, 邵东波, 蔺宏斌.  鄂尔多斯盆地延长组的湖泊风暴沉积 . 沉积学报, 1999, 17(S1): 758-762.
  • 加载中
计量
  • 文章访问数:  931
  • HTML全文浏览量:  0
  • PDF下载量:  1282
  • 被引次数: 0
出版历程
  • 收稿日期:  2013-12-16
  • 修回日期:  2014-03-21
  • 刊出日期:  2014-12-10

目录

    鄂尔多斯盆地延长组湖相黏土岩分类和沉积环境探讨

      基金项目:  国家油气重大专项“岩性地层油气藏成藏规律、关键技术及目标评价”(编号:2011ZX05001)资助
      作者简介:

      刘群 女 1991年出生 硕士研究生 湖盆沉积学与非常规石油地质 E-mail:ro1ql14@abdn.ac.uk

    • 中图分类号: TE121.3+1

    摘要: 鄂尔多斯盆地三叠系延长组长7油层组沉积了区域分布的大套湖相黏土岩,它不但是鄂尔多斯盆地中生界最重要的烃源岩,同时也是目前致密油/页岩油勘探的主要领域.作者在对国内外黏土岩分类及其成因机制等系统调研基础上,通过对工区25口连续取芯井的岩芯描述和400余块典型黏土岩薄片观察,并充分应用X衍射、有机地球化学等分析测试资料,提出了湖相黏土岩的分类方案与基本特征,探讨了不同类型黏土岩形成的沉积环境.根据岩石组分、沉积构造等特征,鄂尔多斯盆地延长组长7油层组黏土岩主要发育5种类型:①块状泥岩;②粒序层理泥岩;③波状纹层页岩;④平直纹层页岩;⑤似块状页岩.该成因分类方案将黏土岩类型与沉积环境相结合.指出受三角洲前缘影响的浅湖区以块状泥岩为主;受湖流和波浪影响的浅湖—半深湖环境以波状纹层页岩为主;深湖静水区以平直纹层状页岩为主;深湖坳陷区以粒序层理泥岩为主;火山灰爆发时期以似块状页岩为主.粒序层理泥岩是致密油赋存的主要类型,有机碳平均含量为6%;似块状页岩是页岩油赋存的主要类型,有机碳平均含量为17.17%.

    English Abstract

    刘群, 袁选俊, 林森虎, 王岚, 郭浩, 潘松圻, 姚泾利. 鄂尔多斯盆地延长组湖相黏土岩分类和沉积环境探讨[J]. 沉积学报, 2014, 32(6): 1016-1025.
    引用本文: 刘群, 袁选俊, 林森虎, 王岚, 郭浩, 潘松圻, 姚泾利. 鄂尔多斯盆地延长组湖相黏土岩分类和沉积环境探讨[J]. 沉积学报, 2014, 32(6): 1016-1025.
    LIU Qun, YUAN Xuan-jun, LIN Sen-hu, WANG Lan, GUO Hao, PAN Song-qi, YAO Jing-li. The Classification of Lacustrine Mudrock and Research on Its' Depositional Environment[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1016-1025.
    Citation: LIU Qun, YUAN Xuan-jun, LIN Sen-hu, WANG Lan, GUO Hao, PAN Song-qi, YAO Jing-li. The Classification of Lacustrine Mudrock and Research on Its' Depositional Environment[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1016-1025.
    参考文献 (38)

    目录

      /

      返回文章
      返回