天然气地球科学

• 天然气地质学 • 上一篇    下一篇

珠江口盆地陆丰地区恩平组层序地层控制的河道构成样式

芮志锋1,邓宏文1,杨小江2,李潇2,郭佳3   

  1. 1.中国地质大学(北京)能源学院,北京 100083;
    2.中海石油(中国)有限公司深圳分公司,广东 深圳 518000;
    3.中海油研究总院,北京 100028
  • 收稿日期:2019-01-03 修回日期:2019-01-29 出版日期:2019-05-10
  • 作者简介:芮志锋(1985-),男,浙江浦江人,在读博士,主要从事盆地分析及层序地层学研究.E-mail:zhifengrui@163.com.
  • 基金资助:
    国家自然科学基金重点项目“南海北部新近纪陆架坡折的发育演化及其对南海盆地动力学过程的沉积响应”(编号: 91328201)资助.

The channel stacking pattern under the control of sequence stratigraphicof Enping Formation in Lufeng area,Pearl River Mouth Basin

Rui Zhi-feng1,Deng Hong-wen1,Yang Xiao-jiang2, Li Xiao2,Guo Jia3   

  1. 1.School of Energy Resources,China University of Geosciences,Beijing 100083,China;
    2.Shenzhen Oil Research Institute,China National Offshore Oilfield Corporation Limited-Shenzhen,Shenzhen 518000,China;3.CNOOC Research Institute,Beijing 100028,China
  • Received:2019-01-03 Revised:2019-01-29 Online:2019-05-10

摘要: 依据河流相层序地层理论,综合利用岩心、测井以及地震资料,开展了陆丰地区恩平组不同层序地层位置河道构成解剖工作,将恩平组划分为3个受可容纳空间变化控制的三级层序,提出了低可容纳空间条件下形成的厚层—叠置的三角洲平原辫状分流河道、中等可容纳空间条件下形成的厚层、叠置—孤立三角洲前缘分支河道以及高可容纳空间条件下形成的薄层、朵叶体上孤立分支河道—席状砂3种不同河道构成样式。不同构成样式河道的油藏特征具有明显的差异。其中,低可容纳空间条件下形成的厚层—叠置的三角洲平原辫状分流河道以构造油气藏为主,高可容纳空间条件下形成的薄层、朵叶体上孤立分支河道以岩性油气藏为主。该分析方法、手段在其他类似地区具有一定的借鉴意义。

关键词: 河道构成样式, 可容纳空间, 层序地层控制, 恩平组, 陆丰地区

Abstract: Based on the integrated utilization of cores,logging and seismic data,and according to the fluvial sequence stratigraphic theory,the channel stacking patterns of Enping Formation were analyzed.Enping Formation was divided into three 3rd-order sequences which were controlled by the variation of accommodation.The three channel stacking patterns were summarized:Thick-stacked delta plain braided distributary channels under low accommodation,thick-stacked or isolated delta front branch channels under middle accommodation,thin-isolated branch channels-sheet sand under high accommodation.Different channel stacking patterns have different reservoir characteristics.The thick-stacked delta plain braided distributary channels under low accommodation mainly formed structural reservoirs,and the thin-isolated branch channels-sheet sand under high accommodation mainly formed lithologic reservoirs.This analysis method has some reference significance for other similar areas.

Key words: Channel stacking pattern, Accommodation, The control of sequence stratigraphic, Enping Formation, Lufeng area

中图分类号: 

  • TE121.3
[1]Qin Guoquan.Late Cenozoic sequence stratigraphy and sea-level changes in Pearl River Mouth Basin,South China Sea[J].China Offshore Oil and Gas:Geology,2002,16(1):1-10.
秦国权.珠江口盆地新生代晚期层序地层划分和海平面变化[J].中国海上油气:地质,2002,16(1):1-10.
[2]Chen Changmin,Shi Hesheng,Xu Shice,et al.Tertiary Hydrocarbon Accumulation Condition in Pearl River Mouth Basin[M].Beijing:Science Press,2003:1-30.
陈长民,施和生,许仕策,等.珠江口盆地(东部)第三系油气藏形成条件[M].北京:科学出版社,2003:1-30.
[3]Shi Hesheng,He Min,Zhang Lili,et al.Hydrocarbon geology,accumulation pattern and the next exploration strategy in the eastern Pearl River Mouth Basin[J].China Offshore Oil and Gas,2014,26(3):11-22.
施和生,何敏,张丽丽,等.珠江口盆地(东部)油气地质特征,成藏规律及下一步勘探策略[J].中国海上油气,2014,26(3):11-22.
[4]Cui Shasha,He Jiaxiong,Chen Shenghong,et al.Development characteristics of Pearl River Mouth Basin and its geological conditions for oil and gas accumulation[J].Natural Gas Geoscience,2009,20(3):384-391.
崔莎莎,何家雄,陈胜红,等.珠江口盆地发育演化特征及其油气成藏地质条件[J].天然气地球科学,2009,20(3):384-391.
[5]Cai Zhourong,Liu Weiliang,Wan Zhifeng,et al.Determination of Cenozoic tectonic movement in the northern South China Sea and the relationship between oil-gas and tectonic movement[J].Marine Science Bulletin,2010,29(2):161-165.
蔡周荣,刘维亮,万志峰,等.南海北部新生代构造运动厘定及与油气成藏关系探讨[J].海洋通报,2010,29(2):161-165.
[6]Liu An,Wu Shimin,Cheng Weihua.Tectonic subsidence history and dynamic mechanism of the Dongsha rise in the Zhujiang River Mouth Basin[J].Journal of Marine,2011,33(6):117-124.
刘安,吴世敏,程卫华.珠江口盆地东沙隆起的沉降史及其动力机制[J].海洋学报,2011,33(6):117-124.
[7]Luo Donghong,Liu Weixin,Dai Zong,et al.Key techniques to evaluate deep reservoir and their application in the eastern Pearl River Mouth Basin[J].China Offshore Oil and Gas,2014,26(3):56-60.
罗东红,刘伟新,戴宗,等.珠江口盆地(东部)深层储层评价关键技术及其应用[J].中国海上油气,2014,26(3):56-60.
[8]Luo Donghong,Liang Wei,Li Xisheng,et al.A breakthrough at Paleogene Enping Formation and its important significance in Lufeng 13-1 Oilfield,Pearl River Mouth Basin[J].China Offshore Oil and Gas,2011,23(2):71-75.
罗东红,梁卫,李熙盛,等.珠江口盆地陆丰13-1油田古近系恩平组突破及其重要意义[J].中国海上油气,2011,23(2):71-75.
[9]Lv Duanchuan,Lin Chengyan,Ren Lihua,et al.Flow unit combination and water flooding model of distributary channel sand body in eastern Xing-6 block[J].Lithologic Reservoirs,2018,30(5):103-108.
吕端川,林承焰,任丽华,等.杏六区东部分流河道砂体渗流单元组合及水淹模式[J].岩性油气藏,2018,30(5):103-108.
[10]Alqahtani F A,Johnson H D,Jackson C A,et al.Nature,origin and evolution of a Late Pleistocene incised valley-fill,Sunda Shelf Southeast Asia[J].Sedimentology,2015,62:1198-2332.
[11]Gouw M J P,Autin W J.Alluvial architecture of the Holocene Lower Mississippi Valley(U.S.A.) and a comparison with the Rhine-Meusedelta(The Netherlands)[J].Sedimentary Geology,2008,204(3/4):106-121.
[12]Hampson G J,RoyhanGani M,Sahoo H,et al.Controls on large-scale patterns of fluvial sandbody distribution in alluvial to coastal plain strata:Upper Cretaceous Blackhawk Formation,Wasatch Plateau,Central Utah,USA[J].Sedimentology,2012,59(7):2226-2258.
[13]Miall A D.Fluvial Depositional Systems[M].Berlin:Springer,2014:322.
[14]Ghinassi M,Nemec W,Aldinucci M,et al.Plan-form evolution of ancient meandering rivers reconstructed from longitudinal outcrop sections[J].Sedimentology,2014,61(4):952-977.
[15]Huerta P,Armenteros I,Silva P G.Large-scale architecture in non-marine basins:The response to the interplay between accommodation space and sediment supply[J].Sedimentology,2011,58(7):1716-1736.
[16]Bai Zhenhua,Zhan Yantao,Wang Ying,et al.Fluvial sand bodies distribution and evolution of He 8 member in Su 14 block of Sulige Gas Field[J].Lithologic Reservoirs,2013,25(1):56-62.
白振华,詹燕涛,王赢,等.苏里格气田苏14井区盒8段河流相砂体展布与演化规律研究[J].岩性油气藏,2013,25(1):56-62.
[17]Si Li.Geological modeling for point bar of meandering river and its application in horizontal well[J].Lithologic Reservoirs,2008,20(3):104-108.
司丽.曲流河点坝砂体地质建模及在水平井轨迹设计中的应用[J].岩性油气藏,2008,20(3):104-108.
[18]Gan Liqin,Su Jinchang,Xie Yue,et al.Interlayers of meandering river reservoir:A case from Qinhuangdao 32-6 Oilfield[J].Lithologic Reservoirs,2017,29(6):128-134.
甘立琴,苏进昌,谢岳,等.曲流河储层隔夹层研究——以秦皇岛32-6 油田为例[J].岩性油气藏,2017,29(6):128-134.
[19]Cui Lianke,Shan Jingfu,Li Fuping,et al.Estimating method of braided channel bar under sparse well net:A case from Su X block in Sulige Gas Field[J].Lithologic Reservoirs,2018,30(1):155-164.
崔连可,单敬福,李浮萍,等.基于稀疏井网条件下的古辫状河道心滩砂体估算——以苏里格气田苏X区块为例[J].岩性油气藏,2018,30(1):155-164.
[20]Su Jinchang,Zhang Lan,Ma Xinfu.Geological modeling in initial stage of development of fluvial reservoir[J].Lithologic Reservoirs,2008,20(3):114-118.
苏进昌,张岚,马新福.河流相储层开发初期地质建模[J].岩性油气藏,2008,20(3):114-118.
[21]Wang Baocheng,Bai Liande.Fluvial stratigraphic sequence development and constitution pattern[J].Special Oil and Gas Reservoirs,2008,15(4):13-17.
王宝成,白连德.河流相地层层序发育特征及构成模式[J].特种油气藏,2008,15(4):13-17.
[22]Chen Fei,Luo Ping,Zhang Xingyang,et al.Stratigraphic architecture and sequence stratigraphy of Upper Triassic Yanchang Formation in the eastern margin of Ordos Basin[J].Earth Science Frontiers,2010,17(1):330-338.
[JP3]陈飞,罗平,张兴阳,等.鄂尔多斯盆地东缘上三叠统延长组砂体结构与层序地层学研究[J].地学前缘,2010,17(1):330-338.
[23]Zhang Changmin,Hu Wei,Zhu Rui,et al.Concept of distributive fluvial system and its significance to oil and gas exploration and development[J].Lithologic Reservoirs,2017,29(3):1-9.
张昌民,胡威,朱锐,等.分支河流体系的概念及其对油气勘探开发的意义[J].岩性油气藏,2017,29(3):1-9.
[24]Sun Tingbin,Guo Dianbin,Li Zhongchao,et al.Distribution characteristics of branch channel of shallow delta in Poyang Lake[J].Lithologic Reservoirs,2015,27(5):144-148.
孙廷彬,国殿斌,李中超,等.鄱阳湖浅水三角洲分支河道分布特征[J].岩性油气藏,2015,27(5):144-148.
[25]Zhang Changmin,Yin Taiju,Li Shaohua,et al.Control of base level cycles on channel sand geometry:A case study on ZaoⅡ-Ⅲ reservoirs,Zaoyuan Oilfield[J].Lithologic Reservoirs,2007,19(4):9-12.
张昌民,尹太举,李少华,等.基准面旋回对河道砂体几何形态的控制作用——以枣园油田孔一段枣Ⅱ—Ⅲ油组为例[J].岩性油气藏,2007,19(4):9-12.
[26]Xu Jie,Dong Ning,Ning Junrui,et al.Sedimentary facies prediction of braided channel of the third member of Shihezi Formation in Daniudi Gasfield,Ordos Basin[J].Lithologic Reservoirs,2011,23(2):90-94.
许杰,董宁,宁俊瑞,等.鄂尔多斯盆地大牛地气田盒3 段辫状河道沉积相预测[J].岩性油气藏,2011,23(2):90-94.
[27]Yang Youxing,Jin Zhenkui,Bai Zhongkai,et al.Contact relationship and main controlling factors of braided river single channel sand body:A case of braided river from Karamay in Xinjiang,Liulin and Datong in Shanxi,Yan’an in Shaanxi[J].Lithologic Reservoirs,2018,30(2):30-38.
杨有星,金振奎,白忠凯,等.辫状河单河道砂体接触关系及主控因素分析——以新疆克拉玛依,山西柳林,大同和陕西延安辫状河露头为例[J].岩性油气藏,2018,30(2):30-38.
[28]Wang Yue,Guo Yanru,Zhang Yanling,et al.Genetic types,configurations and distribution of sand bodies of Shanxi Formation in northeastern Ordos Basin[J].Lithologic Reservoirs,2018,30(3):80-91.
王玥,郭彦如,张延玲,等.鄂尔多斯盆地东北部山西组层序格架下的砂体成因类型,构型及分布[J].岩性油气藏,2018,30(3):80-91.
[29]Li Zhihua,Huang Wenhui.Lithofacies characteristics and sedimentary model of braided delta:A case study of He 8 member in the southern Sulige,Ordos Basin[J].Lithologic Reservoirs,2017,29(1):43-50.
李志华,黄文辉.辫状河三角洲岩相特征及沉积模式——以鄂尔多斯盆地苏南地区盒8段为例[J].岩性油气藏,2017,29(1):43-50.
[30]Chen Fei,Hu Guangyi,Fan Tingen,et al.Sandbody architecture and sequence stratigraphy of fluvial facies,Neogene Minghuazhen formation,W Oilfield,Bohai Bay[J].Earth Science Frontiers,2015,22(2):207-213.
陈飞,胡光义,范廷恩,等.渤海海域W油田新近系明化镇组河流相砂体结构特征[J].地学前缘,2015,22(2):207-213.
[31]Hu Guangyi,Chen Fei,Fan Tingen,et al.Analysis of fluvial facies compound sandbody architecture of the Neogene Minghuazhen Formation of S oilfield in the Bohai Bay[J].Acta Sedimentologica Sinica,2014,32(3):586-592.
胡光义,陈飞,范廷恩,等.渤海海域S油田新近系明化镇组河流相复合砂体叠置样式分析[J].沉积学报,2014,32(3):586-592.
[32]Hu Guangming,Wang Jun,Ji Youliang,et al.Fluvial sequence stratigraphy mode and isochronous strata correlation[J].Acta Sedimentologica Sinica,2010,28(4):745-751.
胡光明,王军,纪友亮,等.河流相层序地层模式与地层等时对比[J].沉积学报,2010,28(4):745-751.
[33]Chen Liuqin,Guo Fusheng,Liang Wei.A review of terrestrial sequence stratigraphy[J].Journal of Stratigraphy,2014,38(2):227-235.
陈留勤,郭福生,梁伟.河流相层序地层学研究现状及发展方向[J].地层学杂志,2014,38(2):227-235.
[34]Zhang Liping,Chen Xuan,Zhang Changmin,et al.Sequence stratigraphy and discipline of lithologic reservoirs for hydrocarbon accumulation in fluvial facies[J].Journal of Jilin University,2010,40(5):1004-1013.
张利萍,陈轩,张昌民,等.河流相层序地层及岩性油气藏油气富集规律[J].吉林大学学报,2010,40(5):1004-1013.
[35]Zheng Rongcai,Yin Shimin,Peng Jun.Sedimentary dynamic analysis of sequence structure and stacking pattern of base level cycle[J].Acta Sedimentologica Sinica,2000,18(3):369-375.
郑荣才,尹世民,彭军.基准面旋回结构与叠加样式的沉积动力学分析[J].沉积学报,2000,18(3):369-375.
[36]Chen Rong,Wang Feng,Li Yong,et al.Sequence stratigraphy and sedimentary filling evolution of fluvial facies of the Neogene of gentle slope belt in Huanghua Depression,Bohai Bay Basin[J].Journal of Paleogeography,2016,18(6):976-985.
陈蓉,王峰,李勇,等.渤海湾盆地黄骅坳陷缓坡带新近系河流相层序发育特征及沉积充填演化[J].古地理学报,2016,18(6):976-985.
[37]Wright V P,Marriott  S B.The sequence stratigraphy of fluvial depositional systems:The role of flood plain sediment storage[J].Sedimentary Geology,1993,86:203-210.
[38]Deng Hongwen,Wang Hongliang,Yan Weipeng,et al.Architecture model of sequence stratigraphy in fluvial facies[J].Acta Sedimentologica Sinica,2004,22(3):373-379.
邓宏文,王红亮,阎伟鹏,等.河流相层序地层构成模式探讨[J].沉积学报,2004,22(3):373-379.
[39]Deng Hongwen,Wu Haibo,Wang Ning,et al.Division of fluvial sequence stratigraphy:An example from the Lower Cretaceous Fuyu oil-bearing layer,the Songliao Basin[J].Oil & Gas Geology,2007,28(5):621-627.
邓宏文,吴海波,王宁,等.河流相层序地层划分方法——以松辽盆地下白主统扶余油层为例[J].石油与天然气地质,2007,28(5):621-627.
[1] 马明, 陈国俊, 李超, 张功成, 晏英凯, 赵钊, 沈怀磊. 珠江口盆地白云凹陷恩平组储层成岩作用与孔隙演化定量表征[J]. 天然气地球科学, 2017, 28(10): 1515-1526.
[2] 郭帅,陈莹,曾清波,杨海长,韩银学,纪沫,沈怀磊,郭佳,赵钊. 珠江口盆地白云凹陷北坡恩平组上段三角洲物源演化及储集意义[J]. 天然气地球科学, 2017, 28(10): 1527-1536.
[3] 刘宝;母国妍;张宁;. 下辽河坳陷西部凹陷下第三系砂体时空展布规律及其主控因素[J]. 天然气地球科学, 2005, 16(6): 747-751.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 王先彬;妥进才;周世新;李振西;张铭杰;闫宏;. 论天然气形成机制与相关地球科学问题[J]. 天然气地球科学, 2006, 17(1): 7 -13 .
[2] 李美俊;卢鸿;王铁冠;吴炜强;刘菊;高黎惠;. 北部湾盆地福山凹陷岩浆活动与CO2 成藏的关系[J]. 天然气地球科学, 2006, 17(1): 55 -59 .
[3] 倪金龙;夏斌;. 济阳坳陷坡折带组合类型及石油地质意义[J]. 天然气地球科学, 2006, 17(1): 64 -68 .
[4] 施立志;林铁锋;王震亮;王卓卓;姚勇;. 库车坳陷下白垩统天然气运聚系统与油气运移研究[J]. 天然气地球科学, 2006, 17(1): 78 -83 .
[5] 唐友军,文志刚,窦立荣,徐佑德. 一种估算原油成熟度的新方法[J]. 天然气地球科学, 2006, 17(2): 160 -162 .
[6] Cramer B;Faber E;Gerling P;Krooss B M;刘全有(译). 天然气稳定碳同位素反应动力学研究――关于干燥、开放热解实验中的思考[J]. 天然气地球科学, 2002, 13(5-6): 8 -18 .
[7] 郭精义,杨占龙,黄刚,杨立国. 潜江凹陷新农地区沉积微相特征与岩性油气藏[J]. 天然气地球科学, 2006, 17(2): 249 -255 .
[8] 张丽娟;李多丽;孙玉善;程明. 库车坳陷西部古近系-白垩系沉积储层特征分析[J]. 天然气地球科学, 2006, 17(3): 355 -360 .
[9] 付广;孟庆芬;. 断层封闭性影响因素的理论分析[J]. 天然气地球科学, 2002, 13(3-4): 40 -44 .
[10] 杨蕾;同登科;. 变形介质煤层气双渗流动压力分析[J]. 天然气地球科学, 2006, 17(3): 429 -433 .