鲁西豫东地区奥陶纪岩相古地理特征及其演化<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2023.01.009

古地理学报 ›› 2023, Vol. 25 ›› Issue (1): 133-148. doi: 10.7605/gdlxb.2023.01.009

• 岩相古地理学及沉积学 • 上一篇下一篇

鲁西豫东地区奥陶纪岩相古地理特征及其演化^*

贾艳雨^1,2, 宿宇驰^3,4, 隋少强^1,2, 贾维明^3,4, 李宗峰^3,4, 杨志波^3,4, 王茜^1,2, 高飞^1,2, 季汉成^3,4, 鲍志东^3,4

1 中国石化新星(北京)新能源研究院有限公司,北京 100083;
2 中国石化地热资源开发利用重点实验室,北京 1000833;
3 中国石油大学(北京)油气资源与探测国家重点实验室,北京 102249;
4 中国石油大学(北京)地球科学学院,北京 102249

收稿日期:2022-10-10 修回日期:2022-12-21 出版日期:2023-02-01 发布日期:2023-02-17
通讯作者: 宿宇驰,男,1994年生,研究方向为沉积学与含油气盆地分析、地热资源分析与评价研究。E-mail: 1219133033@qq.com。贾维明,男,1998年生,研究方向为沉积学与地热资源勘查研究。E-mail: 1522043579@qq.com。
作者简介:贾艳雨,男,1988年生,高级工程师,研究方向为非常规油气地质、地热地质、新能源战略规划工作。E-mail: jiayanyu2007@163.com。
基金资助:
*中国石油化工股份有限公司重点科技项目(编号: JP21005)与国家重点研发计划(编号: 2017YFC0603104,2018YFC0604304)联合资助

Lithofacies palaeogeographic characteristics and evolution of the Ordovician in western Shandong-eastern Henan area

JIA Yanyu^1,2, SU Yuchi^3,4, SUI Shaoqiang^1,2, JIA Weiming^3,4, LI Zongfeng^3,4, YANG Zhibo^3,4, WANG Xi^1,2, GAO Fei^1,2, JI Hancheng^3,4, BAO Zhidong^3,4

1 Star(Beijing)New Energy Research Institute Co. Ltd.,SINOPEC, Beijing 100083,China;
2 Key Laboratory of Geothermal Exploration and Utilization,SINOPEC,Beijing 100083,China;
3 State Key Laboratory of Petroleum Resources and Prospecting,China University of Petroleum(Beijing),Beijing 102249,China;
4 College of Geosciences,China University of Petroleum(Beijing),Beijing 102249,China

Received:2022-10-10 Revised:2022-12-21 Online:2023-02-01 Published:2023-02-17
Contact: SU Yuchi,born in 1994. He is mainly engaged in sedimentology and analysis in petroliferous basins, geothermal resources analysis and evaluation. E-mail: 1219133033@qq.com. JIA Weiming,born in 1998. He is mainly engaged in sedimentology and geothermal resource exploration. E-mail: 1522043579@qq.com.
About author:JIA Yanyu,born in 1988,is a senior engineer. He is mainly engaged in unconventional oil and gas geology,geothermal geology and new energy strategic planning. E-mail: jiayanyu2007@163.com.
Supported by:
Co-funded by the Key Scientific and Technological Project of Sinopec(No. JP21005)and National Key Research and Development Program of China(Nos. 2017YFC0603104,2018YFC0604304)

摘要/Abstract

摘要： 鲁西豫东地区奥陶系碳酸盐岩地层是重要的石油和地下热水储集层。受限于基础地质资料,前人对鲁西豫东地区奥陶系层序划分存在争议,缺少对岩相古地理演化的精细刻画。为明确奥陶系层序地层特征与各期岩相古地理演化特征,通过对鲁西豫东地区周缘野外地质剖面考察、19口井岩心观察以及测井曲线特征分析,在层序地层格架内,对奥陶纪岩相古地理展布及其演化特征进行了研究。结果表明,根据层序界面类型和最大海泛面发育位置,研究区奥陶系可划分为SSQ1-SSQ2共2个二级层序和SQ1-SQ4共4个三级层序; 沉积相类型为海相碳酸盐岩台地,包括局限台地、开阔台地和蒸发台地3种亚相,并进一步细分为灰坪、颗粒滩、泥灰坪、灰-云坪、云坪、潟湖、含膏云坪和膏云坪8种沉积微相; 岩相古地理单元整体表现出陆表海的沉积建造特征,各期旋回性沉积为储集层叠置发育奠定了物质基础,云坪、膏云坪、含膏云坪、颗粒滩微相易于形成有利储集空间,是区域地热资源勘探开发的重点领域。

关键词: 层序地层, 岩相古地理, 奥陶系, 鲁西豫东地区

Abstract: The Ordovician carbonate strata in western Shandong-eastern Henan represent important oil and hot water reservoirs. Limited by the basic geological data,there is controversy over sequence classification of Ordovician carbonate in western Shandong-eastern Henan,the lack of detailed investigation of sedimentary facies and lithofacies palaeogeography. Through the field geological profile investigation of the perimeter of the study area,the core observation of 19 wells in the study area and the analysis of the shape of the logging curve,the lithofacies palaeogeography of Ordovician and its evolution characteristics in the study area were reconstructed,in order to clarify the characteristics of sequence stratigraphy and lithofacies palaeogeography feature in each period of the Ordovician in the study area. Results from the current study suggest that according to the sequence boundaries and the output position of the maximum flooding surface,the Ordovician sedimentary strata were divided into two second-order sequences of SSQ1-SSQ2 and four third-order sequences of SQ1-SQ4. The Ordovician carbonate strata of study area were formed in the marine carbonate platform sedimentary environments,including three subfacies,including restricted platform,open platform and evaporate platform. They were further subdivided into eight sedimentary microfacies,including carbonate flat,grain beach,muddy carbonate flat,carbonate-dolomite flat,dolomite flat,lagoon,gypsum-dolomite flat and gypsum-bearing dolomite flat. The lithofacies palaeogeographic units of SQ1-SQ4 show the sedimentary construction characteristics of land surface seas as a whole,and seawater mainly inflows from the northeast. Dolomite flat,gypsum-dolomite flat,gypsum-bearing dolomite flat,and grain beach microfacies are favorable for the formation of reservoir space,which are the focused areas of regional hydrocarbon and hot water exploration and development.

Key words: sequence stratigraphy, lithofacies palaeogeography, Ordovician, western Shandong-eastern Henan area

中图分类号:

P531

贾艳雨, 宿宇驰, 隋少强, 贾维明, 李宗峰, 杨志波, 王茜, 高飞, 季汉成, 鲍志东. 鲁西豫东地区奥陶纪岩相古地理特征及其演化^*[J]. 古地理学报, 2023, 25(1): 133-148.

JIA Yanyu, SU Yuchi, SUI Shaoqiang, JIA Weiming, LI Zongfeng, YANG Zhibo, WANG Xi, GAO Fei, JI Hancheng, BAO Zhidong. Lithofacies palaeogeographic characteristics and evolution of the Ordovician in western Shandong-eastern Henan area[J]. JOPC, 2023, 25(1): 133-148.

http://www.gdlxb.cn/CN/Y2023/V25/I1/133

参考文献

[1] 曹高社,徐光明,林玉祥,杨启浩. 2013. 华北东部前中生代盆地基底的几何学特征. 河南理工大学学报(自然科学版), 32(1): 46-51.
[Cao G S,Xu G M,Lin Y X,Yang Q H. 2013. Geometry characteristics of pre-mesozoic basin of eastern part of north China. Journal of Henan Polytechnic University(Natural Science), 32(1): 46-51]
[2] 曹红霞,李文厚,吴海燕,王振国,武渝,任星民. 2021. 陕北地区奥陶纪马家沟组五段沉积时期岩相古地理演化. 古地理学报, 23(4): 723-734.
[Cao H X,Li W H,Wu H Y,Wang Z G,Wu Y,R X M. 2021. Lithofacies palaeogeography evolution of the Member 5 of Ordovician Majiagou sedimentary stage in northern Shaanxi Province. Journal of Palaeogeography(Chinese Edition), 23(4): 723-734]
[3] 陈建强,胡树庭,杨欣德. 2001. 山东淄博地区奥陶系层序地层划分和层序界面的识别标志. 现代地质, 15(3): 247-253, 356.
[Chen J Q,Hu S T,Yang X D. 2001. Ordovician sequence stratigraphy and the sequence boundary marks of Zibo,Shandong Province. Geoscience, 15(3): 247-253, 356]
[4] 陈小炜,牟传龙,周恳恳,康建威,王启宇,葛祥英,梁薇. 2015. 华北地区奥陶纪岩相古地理. 沉积与特提斯地质, 35(4): 1-11.
[Chen X W,Mou C L,Zhou K K,Kang J W,Wang Q Y,Ge X Y,Liang W. 2015. Sedimentary facies and palaeogeography of the North China region during the Ordovician. Sedimentary Geology and Tethyan Geology, 35(4): 1-11]
[5] 方宝明. 2006. 山东省地热资源综合信息远景预测. 吉林大学博士论文, 16-22.
[Fang B M. 2006. Perspective prognosis on geothermal resource in synthetic information in Shandong Province. Doctoral dissertation of Jilin Unversity, 16-22]
[6] 房超,季汉成,赵庆,肖菁,向鹏飞. 2020. 东濮地区中奥陶统层序格架及沉积演化. 科学技术与工程, 20(26): 10707-10719.
[Fang C,Ji H C,Zhao Q,Xiao J,Xiang P F. 2020. Sequence stratigraphic framework and sedimentary evolution of the Middle Ordovician in Dongpu area. Science Technology and Engineering, 20(26): 10707-10719]
[7] 冯增昭. 1979. 华北早奥陶世岩相古地理新探. 地质科学, 14(4): 302-313.
[Feng Z Z. 1979. A preliminary discussion on the Lower Ordovician litho-facies and Paleogegeography in North China. Scientia Geologica Sinica, 14(4): 302-313]
[8] 冯增昭. 1986. 华北地台东部晋冀鲁京津地区早奥陶世岩相古地理. 沉积学报, 4(4): 28-40.
[Feng Z Z. 1986. Early Ordovician lithofacies and paleogeography in east north-China platform. Acta Sedimentologica Sinica, 4(4): 28-40]
[9] 冯增昭. 2004. 单因素分析多因素综合作图法: 定量岩相古地理重建. 古地理学报, 6(1): 3-19.
[Feng Z Z. 2004. Single factor analysis and multifactor comprehensive mapping method: reconstruction of quantitative lithofacies palaeogeography. Journal of Palaeogeography(Chinese Edition), 6(1): 3-19]
[10] 何丽娟,胡圣标,汪集旸. 2001. 中国东部大陆地区岩石圈热结构特征. 自然科学进展, 11(9): 72-75.
[He L J,Hu S B,Wang J Y. 2001. Lithosphere thermal structure of eastern China. Progress in Natural Science, 11(9): 72-75]
[11] 侯中健,陈洪德,田景春,覃建雄,彭军. 2001. 层序岩相古地理编图在岩相古地理分析中的应用. 成都理工学院学报, 28(4): 376-382.
[Hou Z J,Chen H D,Tian J C,Qin J X,Peng J. 2001. The application of sequence lithofacies and paleogeography mapping to the analyses of lithofacies-paleogeography. Journal of Chengdu University of Technology(Science & Technology Edition), 28(4): 376-382]
[12] 金振奎,石良,高白水,余宽宏. 2013. 碳酸盐岩沉积相及相模式. 沉积学报, 31(6): 965-979.
[Jin Z K,Shi L,Gao B S,Yu K H. 2013. Carbonate facies and facies Models. Acta Sedimentologica Sinica, 31(6): 965-979]
[13] 李庆平,董仁国,李秀章,杨恩秀,李霞. 2005. 鲁西寒武系—下奥陶统层序地层研究新进展. 地层学杂志, 29(4): 376-380,386.
[Li Q P,Dong R G,Li X Z,Yang E X,Li X. 2005. New advances in the study of the Cambrian to Lower Ordovician sequence-stratigraphy in the west Shandong. Journal of Stratigraphy, 29(4): 376-380,386]
[14] 李增学,李莹,刘海燕,王东东,王平丽,宋广增,李晓静,贾强,赵洪刚. 2021. 岩相古地理优势相方法及应用: 兼谈“广义”与“狭义”岩相古地理及若干新的研究方向. 古地理学报, 23(3): 489-506.
[Li Z X,Li Y,Liu H Y,Wang D D,Wang P L,Song G Z,Li X J,Jia Q,Zhao H G. 2021. Method and application of lithofacies palaeogeographic dominant facies: also discuss the lithofacies palaeogeography in broad and narrow sense and some new research directions. Journal of Palaeogeography(Chinese Edition), 23(3): 489-506]
[15] 林玉祥,赵承锦,朱传真,栾伟娜,吴玉琛,李佳,李秀芹. 2015. 华北地台东部早奥陶世岩相古地理特征. 地球科学与环境学报, 37(6): 1-9.
[Lin Y X,Zhao C J,Zhu C Z,Luan W N,Wu Y C,Li J,Li X Q. 2015. Lithofacies paleogeography characteristics of Early Ordovician in the eastern part of North China Platform. Journal of Earth Sciences and Environmen, 37(6): 1-9]
[16] 林玉祥,朱传真,赵承锦,吴玉琛,李佳,李秀芹. 2016. 华北地台东部中奥陶世岩相古地理特征. 石油实验地质, 38(5): 559-568.
[Lin Y X,Zhao C J,Zhu C Z,Luan W N,Wu Y C,Li J,Li X Q. 2016. Lithofacies palaeogeography of the Middle Ordovician in the eastern North China Platform. Petroleum Geology & Experiment, 38(5): 559-568]
[17] 刘传虎,王永诗,韩宏伟,王学忠. 2013. 济阳坳陷致密砂岩储层油气成藏机理探讨. 石油实验地质, 35(2): 115-119,126.
[Liu C H,Wang Y S,Han H W,Wang X Z. 2013. Hydrocarbon accumulation mechanism of tight sandstone reservoir in Jiyang Depression. Petroleum Geology & Experiment, 35(2): 115-119,126]
[18] 马永生,田海芹. 2006. 华北盆地北部深层层序古地理与油气地质综合研究. 北京: 地质出版社.
[Ma Y S,Tian H Q. 2006. A Comprehensive Study of Deep Layer Paleogeography and Oil and Gas Geology in the Northern North China Basin. Beijing: Geological Publishing House]
[19] 宋奠南. 2001. 对怀远运动的再认识. 山东地质, 17(1): 19-23,51.
[Song D N. 2001. Recognization of Huaiyuan Movement. Shandong Land and Resources, 17(1): 19-23,51]
[20] 吴乾蕃,谢毅真,祖金华,王都. 1988. 华北地热场研究. 中国地震, 4(1): 43-50.
[Wu Q F,Xie Y Z,Zu J H,Wang D. 1988. A study on the geothermal field in north China. Earthquake Research in China, 4(1): 43-50]
[21] 肖菁,季汉成,华南,房超,李海泉,马鹏鹏. 2016. 渤海湾盆地东濮地区奥陶系沉积相特征及其演化. 岩性油气藏, 28(6): 78-87.
[Xiao J,Ji H C,Hua N,Fang C,Li H Q,Ma P P. 2016. Characteristics and evolution of the Ordovician sedimentary facies in Dongpu area,Bohai Bay Basin. Lithologic Reservoirs, 28(6): 78-87]
[22] 徐学蓓. 2010. 鲁西地块奥陶纪岩相古地理研究. 山东科技大学硕士论文, 32-59.
[Xu X P. 2010. Study on lithofacies palaeogeography of Ordovician in Luxi block. Masteral dissertation of Shandong University of Science and Technology,32-59]
[23] 张厚福. 1985. 鲁西隆起下古生界碳酸盐岩古风化壳的储集特征. 石油学报, 6(3): 19-27.
[Zhang H F. 1985. Reservoir characteristics of the weathering crust in carbonate rocks-case of lower paleozoicerathem,west Shandong uprift. Acta Petrolei Sinica, 6(3): 19-27]
[24] Irwin M L. 1965. General principles of clear water in epeiric sea. AAPG Bulletin, 49(4): 445-459.
[25] Meng X H,Ge M,Tucker M E. 1997. Sequence sequence stratigraphy,sealevel changes and depositional systems in the Cambro-Ordovician of the North China carbonate platform. Sedimentary Geology, 114(1): 189-222.
[26] Vail P R,Mitchum Jr R M,Thompson III S. 1977. Seismic stratigraphy and global changes of sea level: Part 3.Relative changes of sea level from Coastal Onlap: section 2. Application of Seismic Reflection Configuration to Stratigrapic Interpretation: 63-81.
[27] Wilson J L. 1975. Carbonate Facies in Geological History. New York: Springer.
[28] Zhen Y Y,Zhang Y D,Wang Z H,Percival I G. 2016. Huaiyuan Epeirogeny-Shaping Ordovician stratigraphy and sedimentation on the North China Platform. Palaeogeography,Palaeoclimatology,Palaeoecology, 448: 363-370.

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[15]	王俊辉, 鲜本忠. 冲积河流平衡的再认识^*[J]. 古地理学报, 2023, 25(5): 1011-1031.

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鲁西豫东地区奥陶纪岩相古地理特征及其演化*

Lithofacies palaeogeographic characteristics and evolution of the Ordovician in western Shandong-eastern Henan area

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鲁西豫东地区奥陶纪岩相古地理特征及其演化^*