岩性油气藏 ›› 2025, Vol. 37 ›› Issue (3): 140–152.doi: 10.12108/yxyqc.20250313

• 地质勘探 • 上一篇    

极缓坡湖盆浅水三角洲前缘砂体类型及成因模式——以鄂尔多斯盆地郝滩地区三叠系长81亚段为例

刘迎宝1,2, 李元昊1,2, 翟文彬1,2, 赵文暄1,2, 李哲3, 杨龙华4, 郭雅倩1,2   

  1. 1. 西安石油大学 地球科学与工程学院, 西安 710065;
    2. 西安石油大学 陕西省油气成藏地质学重点实验室, 西安 710065;
    3. 东方地球物理公司 研究院大庆物探研究院, 黑龙江 大庆 163000;
    4. 陕西银矿矿业有限公司, 陕西 商洛 711405
  • 收稿日期:2024-11-25 修回日期:2024-12-25 发布日期:2025-05-10
  • 第一作者:刘迎宝（2000—），女，西安石油大学在读硕士研究生，研究方向为沉积与储层地质学。地址：（710065）陕西省西安市雁塔区电子二路口东段18号西安石油大学。Email：941085014@qq.com。
  • 通信作者: 李元昊（1976—），男，博士，副教授，主要从事含油气盆地构造、沉积与储层、油藏等方面的教学与研究工作。Email：liyuanh@xsyu.edu.cn。
  • 基金资助:
    国家自然科学基金“盆地晚期-后期差异隆升改造及其油气成藏效应—以鄂尔多斯盆地为例”（编号：42230815）资助。

Types and genetic models of sand bodies in shallow water delta front of extremely gentle slope lake basin：A case study of Chang 81 submember of Triassic in Haotan area，Ordos Basin

LIU Yingbao1,2, LI Yuanhao1,2, ZHAI Wenbin1,2, ZHAO Wenxuan1,2, LI Zhe3, YANG Longhua4, GUO Yaqian1,2   

  1. 1. School of Earth Sciences and Engineering, Xi'an Shiyou University, Xi'an 710065, China;
    2. Shaanxi Key Laboratory of Petroleum Accumulation Geology, Xi'an Shiyou University, Xi'an 710065, China;
    3. Daqing Geophysical Exploration Institute, Research Institute of Eastern Geophysical Company, Daqing 163000, Heilongjiang, China;
    4. Shaanxi Silver Mining Co., Ltd., Shangluo 711405, Shaanxi, China
  • Received:2024-11-25 Revised:2024-12-25 Published:2025-05-10

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摘要： 综合运用岩心、测井、地震等资料，对鄂尔多斯盆地郝滩地区三叠系长81亚段极缓坡浅水三角洲前缘砂体类型及成因模式进行了研究。结果表明：①郝滩地区长8沉积期具有构造稳定、坡度极缓（仅0.03°）、水体较浅、湖岸线迁移摆动幅度大的特征。长81亚段主要发育水下分流河道、河口坝、席状砂3种砂体类型和叠置水下分流河道、叠置水下分流河道—河口坝、叠置河口坝等主要复合叠置砂体类型。②三角洲内前缘近端主要发育水下分流河道砂体，砂体叠置类型以水下分流河道多期叠加为主，河流作用主导，测井曲线主要为箱形或钟形，单期砂体厚度（砂厚> 10 m）较大，平面上呈条带状展布；三角洲内前缘远端主要发育水下分流河道和河口坝砂体，形成了叠置水下分流河道、叠置水下分流河道—河口坝、叠置河口坝3种主要复合叠置砂体类型，河流与湖浪共同作用，测井曲线以箱形、钟形、漏斗形为主，单期砂体（厚度为5～10 m）较厚，平面上呈朵状展布；三角洲外前缘主要发育席状砂体，湖浪作用主导，垂向上表现为多期孤立指形砂体，单期砂体（厚度< 2 m）较薄，平面上呈连片性较好的席状砂体。

关键词: 浅水三角洲前缘, 极缓坡, 水下分流河道, 河口坝, 席状砂, 河流作用, 湖浪作用, 长81亚段, 三叠系, 郝滩地区, 鄂尔多斯盆地

Abstract: Based on core，well logging and seismic data，the sand body types and genetic models of extremely gentle slope shallow water delta front of Chang 81 submember of Triassic in Ordos Basin were studied. The results show that：（1）Sedimentary period of Chang 8 in Haotan area is characterized by stable structure，very slow slope（only 0.03°），shallow water and large shoreline migration and swing. Chang 81 submember mainly develops three types of sand bodies：underwater distributary channel，mouth bar，sheet sand，and composite superimposed sand bodies types such as overlapped underwater distributary channel，overlapped underwater distributary channel-mouth bar，and overlapped mouth bar.（2）The proximal delta inner front mainly develops underwater distributary channel sand bodies，and the type of superposition of sand bodies is dominated by multistage superposition of underwater distributary channels，dominated by fluvial action. The logging curves are mainly box or bell shapes，and the thickness of single stage sand bodies（sand thickness > 10 m）is large，with plane distribution in strip. The distal delta inner front mainly develops underwater distributary channels and mouth bar sand bodies，forming three main types of composite superimposed sand bodies types such as overlapped underwater distributary channels，overlapped underwater distributary channel-mouth bars and overlapped mouth bars. The river and lake waves act together. The logging curve shapes are mainly box，bell and funnel， and the single-stage sand body（with a thickness of 5-10 m）is relatively thick，with plane distribution of lobate delta.The outer front of the delta dominated by the action of lake waves mainly develops sheet sand bodies. Vertically，they exhibit multi-stage isolated finger shaped sand bodies，the single-stage sand bodies（thickness < 2 m） are relatively thin，and plane distribution appear as well connected sheet sand bodies.

Key words: shallow water delta front, extremely gentle slope, underwater distributary channel, mouth bar, sheet sand, fluvial action, lake wave action, Chang 81 submember, Triassic, Haotan area, Ordos Basin

中图分类号: 

  • TE121.3
[1] FISK H N,KOLB C R,MCFARLAN E,et al. Sedimentary framework of the modern Mississippi delta[J]. Journal of Sedimentary Research,1954,24(2):76-99.
[2] POSTMA G. An analysis of the variation in delta architecture[J]. Terra Nova,1990,2(2):124-130.
[3] DONALDSON A C. Pennsylvanine sedimentation of central Appalachians[J]. Geological Society of America Special Papers,1974, 148:47-48.
[4] 楼章华,卢庆梅,蔡希源,等. 湖平面升降对浅水三角洲前缘砂体形态的影响[J]. 沉积学报,1998,16(4):27-31. LOU Zhanghua,LU Qingmei,CAI Xiyuan,et al. Influence of lake level fluctuation on sandbody shapes at shallow-water delta front[J]. Acta Sedimentologica Sinica,1998,16(4):27-31.
[5] 邹才能,赵文智,张兴阳,等. 大型敞流坳陷湖盆浅水三角洲与湖盆中心砂体的形成与分布[J]. 地质学报,2008,82(6):813-825. ZOU Caineng,ZHAO Wenzhi,ZHANG Xingyang,et al. Formation and distribution of shallow-water deltas and centralbasin sandbodies in large open depression lake basins[J]. Acta Geologica Sinica,2008,82(6):813-825.
[6] 李元昊,刘池洋,独育国,等. 鄂尔多斯盆地西北部上三叠统延长组长8油层组浅水三角洲沉积特征及湖岸线控砂[J]. 古地理学报,2009,11(3):265-274. LI Yuanhao,LIU Chiyang,DU Yuguo,et al. Sedimentary characteristics of shallow water delta and lake shoreline control on sandbodies of Chang 8 oil-bearing interval of the Upper Triassic Yanchang Formation in northwestern Ordos Basin[J]. Journal of Palaeogeography(Chinese Edition),2009,11(3):265-274.
[7] 朱筱敏,刘媛,方庆,等.大型坳陷湖盆浅水三角洲形成条件和沉积模式:以松辽盆地三肇凹陷扶余油层为例[J]. 地学前缘,2012,19(1):89-99. ZHU Xiaomin,LIU Yuan,FANG Qing,et al. Formation and sedimentary model of shallow delta in large-scale lake:Example from Cretaceous Quantou Formation in Sanzhao Sag, Songliao Basin[J]. Earth Science Frontiers,2012,19(1):89-99.
[8] 王建功,王天琦,卫平生,等. 大型坳陷湖盆浅水三角洲沉积模式:以松辽盆地北部葡萄花油层为例[J]. 岩性油气藏, 2007,19(2):28-34. WANG Jiangong,WANG Tianqi,WEI Pingsheng,et al. Sedimentary mode of shallow lacustrine delta of large continental basin:An example from Putaohua Formation in northern Songliao Basin[J]. Lithologic Reservoirs,2007,19(2):28-34.
[9] 罗浩渝,陈军,章学岐,等. 河控浅水三角洲前缘沉积特征及对岩性油藏的控制:以库车坳陷南斜坡巴西改组为例[J]. 岩性油气藏,2021,33(5):70-80. LUO Haoyu,CHEN Jun,ZHANG Xueqi,et al. Sedimentary characteristics of fluvial dominated shallow water delta front and its control on lithologic reservoir:A case study of Baxigai Formation in south slope of Kuqa Depression[J]. Lithologic Reservoirs,2021,33(5):70-80.
[10] 朱茂,朱筱敏,曾洪流,等. 冀中坳陷饶阳凹陷浅水曲流河三角洲沉积体系:以赵皇庄-肃宁地区沙一段为例[J].岩性油气藏,2017,29(2):59-67. ZHU Mao,ZHU Xiaomin,ZENG Hongliu et al. Depositional system of shallow-water meandering river delta:A case from the first member of Shahejie Formation in ZhaohuangzhuangSuning area of Raoyang Sag,Jizhong Depression[J]. Lithologic Reservoirs,2017,29(2):59-67.
[11] 张新涛,周心怀,李建平,等. 敞流沉积环境中"浅水三角洲前缘砂体体系"研究[J]. 沉积学报,2014,32(2):260-269. ZHANG Xintao,ZHOU Xinhuai,LI Jianping,et al. Unconfined flow deposits in front sandbodies of shallow water deltaic distributary systems[J]. Acta Sedimentologica Sinica,2014,32(2):260-269.
[12] 邱隆伟,杨保良,张阳,等. 湖泊水位对三角洲前缘主要砂体类型的影响:以鄂尔多斯盆地神木地区侏罗系延安组剖面为例[J]. 古地理学报,2016,18(6):939-950. QIU Longwei,YANG Baoliang,ZHANG Yang,et al. Lake level effect on main sandbodies of delta front:A case study from outcrops of the Jurassic Yan'an Formation in Shenmu area,Ordos Basin[J]. Journal of Palaeogeography(Chinese Edition),2016,18(6):939-950.
[13] RITCHIE B,GAWTHORPE R,HARDY S. Three-dimensional numerical modeling of deltaic depositional sequences 2:Influence of local controls[J]. Journal of Sedimentary Research, 2004,74(2):221-238.
[14] NICHOLS G J,FISHER J A. Processes,facies and architecture of fluvial distributary system deposits[J]. Sedimentary Geology,2007,195(1/2):75-90.
[15] 张昌民,尹太举,朱永进,等. 浅水三角洲沉积模式[J]. 沉积学报,2010,28(5):933-944. ZHANG Changmin,YIN Taiju,ZHU Yongjin,et al. Shallow-water deltas and models[J]. Acta Sedimentologica Sinica,2010,28(5):933-944.
[16] 任奕霖,赵俊峰,陈佳宇,等. 鄂尔多斯盆地浅水三角洲前缘沉积特征与砂体构型:以宜川仕望河剖面长9 油层组为例[J]. 新疆石油地质,2022,43(3):310-319. REN Yilin,ZHAO Junfeng,CHEN Jiayu,et al. Sedimentary characteristics and sand body architecture of shallow water delta front in Ordos Basin:A case study of Chang 9 member in Shiwanghe section in Yichuan[J]. Xinjiang Petroleum Geology, 2022,43(3):310-319.
[17] 吕晓光,李长山,蔡希源,等. 松辽大型浅水湖盆三角洲沉积特征及前缘相储层结构模型[J]. 沉积学报,1999,17(4):75-80. LYU Xiaoguang,LI Changshan,CAI Xiyuan,et al. Depositional characteristics and front facies reservoir framework model in Songliao shallow lacustrine delta[J]. Acta Sedimentologica Sinica,1999,17(4):75-80.
[18] 张家强,李士祥,周新平,等. 志丹地区长82砂层组缓坡浅水三角洲前缘砂体发育模式及成因[J]. 岩性油气藏,2020,32(1):36-50. ZHANG Jiaqiang,LI Shixiang,ZHOU Xinping,et al. Development pattern and genesis of gentle slope shallow water delta front sand bodies of Chang 82 sand set in Zhidan area,Ordos Basin[J]. Lithologic Reservoirs,2020,32(1):36-50.
[19] 韩永林,王成玉,王海红,等. 姬塬地区长8油层组浅水三角洲沉积特征[J]. 沉积学报,2009,27(6):1057-1064. HAN Yonglin,WANG Chengyu,WANG Haihong,et al. Sedimentary characteristics of shallow-water deltas in Chang-8 subsection of Yanchang Formation,Jiyuan area[J]. Acta Sedimentologica Sinica,2009,27(6):1057-1064.
[20] 张兴阳,罗平,顾家裕,等. 三级基准面旋回内三角洲砂体骨架模型的建立:以陕北安塞三角洲露头为例[J]. 沉积学报, 2006,23(4):540-548. ZHANG Xingyang,LUO Ping,GU Jiayu,et al. Establishment of the delta sandbody framework model in a 3rd order baselevel cycle:Taking Shanbei Ansai delta outcrop as example[J]. Acta Sedimentologica Sinica,2006,23(4):540-548.
[21] 刘翰林,邱振,徐黎明,等. 鄂尔多斯盆地陇东地区三叠系延长组浅水三角洲砂体特征及厚层砂体成因[J]. 石油勘探与开发,2021,48(1):106-117. LIU Hanlin,QIU Zhen,XU Liming,et al. Distribution of shallow water delta sand bodies and the genesis of thick layer sand bodies of the Triassic Yanchang Formation,Longdong Area,Ordos Basin[J]. Petroleum Exploration and Development,2021, 48(1):106-117.
[22] 赵贤正,金凤鸣,刘震,等. 二连盆地地层岩性油藏"多元控砂-四元成藏-主元富集"与勘探实践(Ⅰ):"多元控砂"机理[J]. 岩性油气藏,2007,19(2):9-15. ZHAO Xianzheng,JIN Fengming,LIU Zhen,et al. "Multifactor controlling,four-factor entrapping and key-factor enrichment" of stratigraphic-lithologic reservoirs and exploration practice in Erlian Basin(Ⅰ): "Multi-factor controlling" mechanism[J]. Lithologic Reservoirs,2007,19(2):9-15.
[23] 李元昊,宋方新,韩鹏,等. 构造稳定时期河控三角洲三元控砂模式[J]. 古地理学报,2019,21(3):397-406. LI Yuanhao,SONG Fangxin,HAN Peng,et al. A ternary sand control model of river-dominated delta in tectonic stability period[J]. Journal of Palaeogeography(Chinese Edition),2019, 21(3):397-406.
[24] 刘君龙,纪友亮,杨克明,等. 浅水湖盆三角洲岸线控砂机理与油气勘探意义:以川西坳陷中段蓬莱镇组为例[J]. 石油学报,2015,36(9):1060-1073. LIU Junlong,JI Youliang,YANG Keming,et al. Mechanism of lake shoreline control on shoal water deltaic sandbodies and its significance for petroleum exploration:A case study of Penglaizhen Formation in the middle part of western Sichuan depression[J]. Acta Petrolei Sinica,2015,36(9):1060-1073.
[25] 刘桂珍,高伟,张丹丹,等. 姬塬地区长81亚油层组浅水型三角洲砂体结构及成因[J]. 岩性油气藏,2019,31(2):16-23. LIU Guizhen,GAO Wei,ZHANG Dandan,et al. Sandbody structure and its genesis of shallow-water delta of Chang 81 reservoir in Jiyuan area,Ordos Basin[J]. Lithologic Reservoirs, 2019,31(2):16-23.
[26] 段悦,侯长冰,郑荣才,等. 镇原地区长8油层组层序-岩相古地理特征及砂体展布规律[J]. 岩性油气藏,2014,26(1):36-44. DUAN Yue,HOU Changbing,ZHENG Rongcai,et al. Sequencebased lithofacies paleogeography and sand body distribution of Chang 8 oil reservoir set in Zhenyuan area,Ordos Basin[J]. Lithologic Reservoirs,2014,26(1):36-44.
[27] YANG Renchao,JIN Zhijun,VAN LOON A J T,et al. Climatic and tectonic controls of lacustrine hyperpycnite origination in the Late Triassic Ordos Basin,central China:Implications for unconventional petroleum development[J]. AAPG Bulletin, 2017,101(1):95-117.
[28] 李树同,王琪,仲佳爱,等. 鄂尔多斯盆地姬塬地区长81浅水三角洲砂体成因[J]. 天然气地球科学,2013,24(6):1102-1108. LI Shutong,WANG Qi,ZHONG Jiaai,et al. The genesis of sandbody in the shallow delta from Chang 81 of Jiyuan area in Ordos Basin[J]. Natural Gas Geoscience,2013,24(6):1102-1108.
[29] 牟蜚声,尹相东,胡琮,等. 鄂尔多斯盆地陕北地区三叠系长7段致密油分布特征及控制因素[J]. 岩性油气藏,2024,36(4):71-84. MOU Feisheng,YIN Xiangdong,HU Cong,et al. Distribution characteristics and controlling factors of tight oil of Triassic Chang 7 member in northern Shaanxi area,Ordos Basin[J]. Lithologic Reservoirs,2024,36(4):71-84.
[30] 郭艳琴. 鄂尔多斯盆地三叠系延长组致密储层特征及油藏富集规律[M]. 北京:石油工业出版社,2016. GUO Yanqin. Tight reservoir characteristics and reservoir enrichment rule of Triassic Yanchang Formation in Ordos Basin[M]. Beijing:Petroleum Industry Press,2016.
[31] 李元昊. 鄂尔多斯盆地延长组下组合石油成藏机理及主控因素[M]. 北京:中国石化出版社,2022:6. LI Yuanhao. Petroleum accumulation mechanism and main controlling factors of lower Yanchang Formation in Ordos Basin[M]. Beijing:China Petrochemical Press,2022:6.
[32] 吉利明,吴涛,李林涛. 陇东三叠系延长组主要油源岩发育时期的古气候特征[J]. 沉积学报,2006,24(3):426-431. JI Liming,WU Tao,LI Lintao. Paleoclimatic characteristics during sedimentary period of main source rocks of Yanchang Formation(Triassic)in eastern Gansu[J]. Acta Sedimentologica Sinica,2006,24(3):426-431.
[33] 范萌萌,卜军,赵筱艳,等. 鄂尔多斯盆地东南部延长组微量元素地球化学特征及环境指示意义[J]. 西北大学学报(自然科学版),2019,49(4):633-642. FAN Mengmeng,BU Jun,ZHAO Xiaoyan,et al. Geochemical characteristics and environmental implications of trace elements of Yanchang Formation in southeastern Ordos Basin[J]. Journal of Northwest University(Natural Science Edition), 2019,49(4):633-642.
[34] 张译丹,姜在兴,杜克峰,等. 鄂尔多斯盆地志丹-富县地区三叠系延长组长8 油层组风暴沉积特征及意义[J]. 石油学报,2019,40(7):813-822. ZHANG Yidan,JIANG Zaixing,DU Kefeng,et al. Sedimentary characteristics and significances of storm deposition in Chang-8 oil layer of Triassic Yanchang Formation,Zhidan-Fuxian area,Ordos Basin[J]. Acta Petrolei Sinica,2019,40(7):813-822.
[35] 于兴河,李胜利,李顺利. 三角洲沉积的结构-成因分类与编图方法[J]. 沉积学报,2013,31(5):782-797. YU Xinghe,LI Shengli,LI Shunli. Textrue-genetic classifications and mapping methods for deltaic deposits[J]. Acta Sedimentologica Sinica,2013,31(5):782-797.
[36] 邓秀芹,罗安湘,张忠义,等. 秦岭造山带与鄂尔多斯盆地印支期构造事件年代学对比[J]. 沉积学报,2013,31(6):939-953. DENG Xiuqin,LUO Anxiang,ZHANG Zhongyi,et al. Geochronological comparison on Indosinian tectonic events between Qinling Orogeny and Ordos Basin[J]. Acta Sedimentologica Sinica,2013,31(6):939-953.
[37] 魏永佩,陈会鑫. 沉积盆地碎屑岩原始厚度恢复经验图版:一种快速实用的方法[J].石油与天然气地质,1999,20(1):90-93. WEI Yongpei,CHEN Huixin. Recovering plate on initial thickness of clastic rocks in sedimentary basins:A quick and practical method[J]. Oil & Gas Geology,1999,20(1):90-93.
[38] 刘化清,李相博,完颜容,等. 鄂尔多斯盆地长8油层组古地理环境与沉积特征[J]. 沉积学报,2011,29(6):1086-1095. LIU Huaqing,LI Xiangbo,WANYAN Rong,et al. Palaeogeographic and sedimentological characteristics of the Triassic Chang 8,Ordos Basin,China[J]. Acta Sedimentologica Sinica, 2011,29(6):1086-1095.
[39] 易定红,石亚军,刘俊丰,等. 柴达木盆地南八仙地区渐新世浅水三角洲物源及沉积演化[J]. 地质学报,2024,98(2):494-510. YI Dinghong,SHI Yajun,LIU Junfeng,et al. Provenance analysis and sedimentary evolution of Oligocene shallow water delta in the Nanbaxian area,northern Qaidam basin[J]. Acta Geologica Sinica,2024,98(2):494-510.
[40] 邓秀芹,楚美娟,王龙,等. 中晚三叠世鄂尔多斯盆地两期沉降及其形成机制[J]. 石油勘探与开发,2024,51(3):501-512. DENG Xiuqin,CHU Meijuan,WANG Long,et al. Two stages of subsidence and its formation mechanisms in Mid-Late Triassic Ordos Basin,NW China[J]. Petroleum Exploration and Development,2024,51(3):501-512.
[41] 杨征,吴胜和,段冬平,等. 西湖凹陷花港组浅水三角洲平原分流河道沉积构型[J]. 古地理学报,2024,26(3):525-544. YANG Zheng,WU Shenghe,DUAN Dongping,et al. Architecture characteristics of distributary channels in shallow water delta plain of the Huagang Formation in Xihu sag,East China Sea[J]. Journal of Palaeogeography(Chinese Edition),2024, 26(3):525-544.
[42] 朱筱敏,赵东娜,曾洪流,等. 松辽盆地齐家地区青山口组浅水三角洲沉积特征及其地震沉积学响应[J]. 沉积学报, 2013,31(5):889-897. ZHU Xiaomin,ZHAO Dongna,ZENG Hongliu,et al. Sedimentary characteristics and seismic sedimentologic responses of shallow-water delta of Qingshankou Formation in Qijia area, Songliao Basin[J]. Acta Sedimentologica Sinica,2013,31(5):889-897.
[43] 袁选俊,周红英,张志杰,等. 坳陷湖盆大型浅水三角洲沉积特征与生长模式[J]. 岩性油气藏,2021,33(1):1-11. YUAN Xuanjun,ZHOU Hongying,ZHANG Zhijie,et al. Depositional features and growth pattern of large shallow-water deltas in depression basin[J]. Lithologic Reservoirs,2021,33(1):1-11.
[44] 卫平生,潘树新,王建功,等. 湖岸线和岩性地层油气藏的关系研究:论"坳陷盆地湖岸线控油"(为《岩性油气藏》创刊而作)[J]. 岩性油气藏,2007,19(1):27-31. WEI Pingsheng,PAN Shuxin,WANG Jiangong,et al. Study of the relationship between lithostratigraphic reservoirs and lakeshore line:Introduction on lakeshore line controlling oil/gas reservoirs in sag basin[J]. Lithologic Reservoirs,2007,19(1):27-31.
[45] 姜在兴,王俊辉,张元福,等."风-源-盆"三元耦合油气储集体预测方法及其应用:对非主力物源区储集体的解释与预测[J]. 石油学报,2020,41(12):1465-1476. JIANG Zaixing,WANG Junhui,ZHANG Yuanfu,et al. Ternary "Windfield-Source-Basin" system for the prediction of hydrocarbon reservoirs:Interpretation and prediction of hydrocarbon reservoirs deviated from the main provenance areas[J]. Acta Petrolei Sinica,2020,41(12):1465-1476.
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