岩性油气藏 ›› 2024, Vol. 36 ›› Issue (3): 117–126.doi: 10.12108/yxyqc.20240311

• 地质勘探 • 上一篇    下一篇

鄂尔多斯盆地二叠系盒8段河流扇沉积模式及勘探意义

王宏波1, 张雷2, 曹茜2, 张建伍2, 潘星2   

  1. 1. 中国石油勘探开发研究院 西北分院, 兰州 730020;
    2. 中国石油长庆油田公司 勘探开发研究院, 西安 710018
  • 收稿日期:2023-08-21 修回日期:2023-09-20 出版日期:2024-05-01 发布日期:2024-04-30
  • 第一作者:王宏波（1975—），男，博士，高级工程师，主要从事石油地质与沉积学方面的研究工作。地址:（730020）甘肃省兰州市城关区雁儿湾路 535 号。Email:wang_hb1@petroChina.com.cn。
  • 通信作者: 张雷（1983—），男，硕士，高级工程师，主要从事石油地质方面的研究工作。Email:zhanglei01_cq@petroChina.com.cn。
  • 基金资助:
    中国石油天然气股份有限公司“十四五”前瞻性基础性重大科技项目“致密气新区新领域资源潜力与富集规律研究”（编号：2021DJ2101）资助。

Sedimentary model of fluvial fan of Permian He-8 member in Ordos Basin and its exploration significance

WANG Hongbo1, ZHANG Lei2, CAO Qian2, ZHANG Jianwu2, PAN Xing2   

  1. 1. PetroChina Research Institute of Petroleum Exploration & Development-Northwest, Lanzhou 730020, China;
    2. Research Institute of Exploration and Development, PetroChina Changqing Oilfield Company, Xi'an 710018, China
  • Received:2023-08-21 Revised:2023-09-20 Online:2024-05-01 Published:2024-04-30

PDF (PC)

181

摘要： 根据野外露头及岩心的分析化验资料，在源-汇系统分析的基础上，对鄂尔多斯盆地二叠系盒 8 段的古气候环境及沉积相特征进行了详细研究。研究结果表明：①鄂尔多斯盆地二叠系盒 8 段 Sr/Cu 的值多大于 10，V/Cr 值多小于 2.0，地层厚度差小于 30 m，未出现明显的突变，古沉积坡度为 0.5°~1.0°，古地貌开阔平缓且无明显坡折带，沉积水体较浅，是在古气候干旱、古地形平缓的背景下，受阶段性洪水作用主导的事件沉积。②盒 8 段沉积期，盆地不存在大面积汇水区，沉积体系中河流并未进入湖泊水体，而是向东南流出盆地或是消失在内陆干旱地区，全盆地以洪泛平原沉积为主，表现为河道与泛滥平原交互分布的沉积格局，形成了河流扇沉积模式。③湖水进退往复，洪水期与枯水期间歇发育，洪水期多期次决口河道接力搬运使得粗粒级砂岩向湖盆长距离延伸，枯水期发育厚层泥质沉积可作为区域性盖层，形成了良好的储盖组合，勘探潜力大。

关键词: 河流扇, 干旱气候, 事件沉积, 洪泛平原, 洪水期, 枯水期, 源-汇系统, 盒8段, 二叠系, 鄂尔多斯盆地

Abstract: Based on the analysis and laboratory data of field outcrops and drilling cores, combined with sourcesink system analysis, the paleoclimatic environment and sedimentary facies characteristics of the eighth member of Permian Shihezi Formation（He-8 member）in Ordos Basin were studied.The results show that:（1）The Sr/ Cu values of Permian He-8 member in Ordos Basin are mostly greater than 10, and the V/Cr values are mostly less than 2.0. The thickness difference of the strata is less than 30 m, and there is no obvious sudden change. The ancient sedimentary slope is 0.5°-1.0°, the paleotopography is open and flat without obvious slope breaks, and the sedimentary water is shallow. It is an event deposit dominated by flood transportation under the background of arid ancient climate and gentle paleotopography.（2）During the sedimentary period of He-8 member, there was no large catchment area in the basin, and the rivers in the sedimentary system did not enter the lake water body. Instead, they flowed out of the basin to the southeast or disappeared in inland arid areas. The entire basin was dominated by floodplain sedimentation, manifested as a sedimentation pattern of alternating distribution of rivers and floodplains, forming afluvial fan sedimentary model.（3）The lake water flows back and forth, with intermittent development in flood season and dry season. In flood season, the relay transport of multi-stage crevasses makes the coarse-grained sandstone extend to the lake basin for a long distance, while in dry season, thick muddy deposits can be used as regional caprocks, forming a good reservoir-cap assemblage with great exploration potential.

Key words: fluvial fan, arid climate, event deposit, floodplain, flood season, dry season, source-sink system, He 8 member, Permian, Ordos Basin

中图分类号: 

  • TE121.3
[1] 杨华,付金华,刘新社,等. 鄂尔多斯盆地上古生界致密气成藏条件与勘探开发[J]. 石油勘探与开发,2012,39(3):295-303. YANG Hua,FU Jinhua,LIU Xinshe,et al. Accumulation conditions and exploration and development of tight gas in the Upper Paleozoic of the Ordos Basin[J]. Petroleum Exploration and Development,2012,39(3):295-303.
[2] 杨西燕,沈昭国,方少仙,等. 鄂尔多斯盆地乌审旗气田中二叠统下石盒子组盒8段下亚段滩坝砂体沉积特征[J]. 古地理学报,2007,9(2):175-183. YANG Xiyan,SHEN Zhaoguo,FANG Shaoxian,et al. Sedimentary characteristics of beach and bar sand bodies in the lower submember of member 8 of Xiashihezi Formation of Middle Permian in Wushenqi gas field,Ordos Basin[J]. Journal of Palaeogeography,2007,9(2):175-183.
[3] 文华国,郑荣才,高红灿,等. 苏里格气田苏6井区下石盒子组盒8段沉积相特征[J]. 沉积学报,2007,25(1):90-98. WEN Huaguo,ZHENG Rongcai,GAO Hongcan,et al. Sedimentary facies of the 8th member of lower Shihezi Formation in Su6 area,Sulige gas field[J]. Acta Sedimentologica Sinica, 2007,25(1):90-98.
[4] 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. 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.
[5] 李洁,陈洪德,侯中健,等. 鄂尔多斯盆地东北部下石盒子组盒8段辫状河三角洲沉积特征[J]. 沉积与特提斯地质,2008, 28(1):27-32. LI Jie,CHEN Hongde,HOU Zhongjian,et al. Sedimentary characteristics of the braided deltas in the eighth member of theLower Shihezi Formation in the northeastern part of the Ordos Basin[J]. Sedimentary Geology and Tethyan Geology,2008,28(1):27-32.
[6] 沈玉林,郭英海,李壮福. 鄂尔多斯盆地苏里格庙地区二叠系山西组及下石盒子组盒八段沉积相[J]. 古地理学报,2006,8(1):53-62. SHEN Yulin,GUO Yinghai,LI Zhuangfu. Sedimentary facies of the Shanxi Formation and member 8 of Xiashihezi Formation of Permian in Suligemiao area,Ordos Basin[J]. Journal of Palaeogeography,2006,8(1):53-62.
[7] 王超勇,陈孟晋,汪泽成,等. 鄂尔多斯盆地南部二叠系山西组及下石盒子组盒8段沉积相[J]. 古地理学报,2007,9(4):369-378. WANG Chaoyong,CHEN Mengjin,WANG Zecheng,et al. Sedimentary facies of the Shanxi Formation and member 8 of Xiashihezi Formation of Permian in southern Ordos Basin[J]. Journal of Palaeogeography,2007,9(4):369-378.
[8] 刘锐娥,肖红平,范立勇,等. 鄂尔多斯盆地二叠系"洪水成因型"辫状河三角洲沉积模式[J]. 石油学报,2013,34(增刊1):120-127. LIU Rui'e,XIAO Hongping,FAN Liyong,et al. A depositional mode of flood-induced braided river delta in Permian of Ordos Basin[J]. Acta Petrolei Sinica,2013,34(Suppl1):120-127.
[9] 肖红平,刘锐娥,张福东,等.鄂尔多斯盆地二叠系盒8段沉积模式重建及其勘探意义[J]. 石油勘探与开发,2019,46(2):268-280. XIAO Hongping,LIU Rui'e,ZHANG Fudong,et al. Sedimentary model reconstruction and exploration significance of Permian He 8 member in Ordos Basin,NW China[J]. Petroleum Exploration and Development,2019,46(2):268-280.
[10] 何自新.鄂尔多斯盆地演化与油气[M].北京:石油工业出版社,2003. HE Zixin. The evolution of Ordos Basin and its oil and gas[M]. Beijing:Petroleum Industry Press,2003.
[11] 翟咏荷,何登发,开百泽.鄂尔多斯盆地及邻区中-晚二叠世构造-沉积环境与原型盆地演化[J]. 岩性油气藏,2024,36, (1):32-44. ZHAI Yonghe,HE Dengfa,KAI Baize. Tectonic-depositional environment and prototype basin evolution of Middle-Late Permian in Ordos Basin and adjacent areas[J]. Lithologic Reservoirs,2024,36(1):32-44.
[12] 王世成,郭亚斌,杨智,等. 苏里格南部盒8 段沉积微相研究[J]. 岩性油气藏,2010,22(增刊1):31-36. WANG Shicheng,GUOYabin,YANG Zhi,et al. Study on sedimentary microfacies of the eighth member of Shihezi Formation in southern Sulige[J].Lithologic Reservoirs,2010,22(Suppl 1):31-36.
[13] 李森,朱如凯,崔景伟,等. 古环境与有机质富集控制因素研究:以鄂尔多斯盆地南缘长7 油层组为例[J]. 岩性油气藏, 2019,31(1):87-95.LI Shen,ZHU Rukai,CUI Jingwei,et al. Paleoenvironment and controlling factors of organic matter enrichment:A case of Chang 7 oil reservoir in southern margin of Ordos Basin[J]. Lithologic Reservoirs,2019,31(1):87-95.
[14] 罗锦昌,田继军,马静辉,等. 吉木萨尔凹陷吉页1井区二叠系芦草沟组沉积环境及有机质富集机理[J]. 岩性油气藏, 2022,34(5):73-85. LUO Jinchang,TIAN Jijun,MA Jinghui,et al. Sedimentary environment and organic matter enrichment mechanism of Permian Lucaogou Formation in Jiye-1 well area,Jimsar Sag[J]. Lithologic Reservoirs,2022,34(5):73-85.
[15] 张元福,戴鑫,王敏,等. 河流扇的概念、特征及意义[J]. 石油勘探与开发,2020,47(5):947-957. ZHANG Yuanfu,DAI Xin,WANG Min,et al. The concept, characteristics and significance of fluvial fans[J]. Petroleum Exploration and Development,2020,47(5):947-957.
[16] 刘宗堡,张云峰,刘云燕,等. 末端扇沉积体系研究现状及石油地质意义[J]. 中国矿业大学学报,2018,47(3):520-530. LIU Zongbao,ZHANG Yunfeng,LIU Yunyan,et al. Status quo of the terminal fan sedimentary system study and its petroleum geological significance[J]. Journal of China University of Mining & Technology,2018,47(3):520-530.
[17] 李相博,刘化清,邓秀芹,等. 干旱环境河流扇概念与鄂尔多斯盆地延长组"满盆砂"成因新解[J]. 沉积学报,2021,39(5):1208-1221. LI Xiangbo,LIU Huaqing,DENG Xiuqin,et al. The concept of fluvial fans in an arid environment:A new explanation of the origin of "sand-filled basins"in the Yanchang Formation,Ordos Basin[J]. Acta Sedimentologica Sinica,2021,39(5):1208-1221.
[18] 肖建新,孙粉锦,何乃祥,等. 鄂尔多斯盆地二叠系山西组及下石盒子组8段南北物源沉积汇水区与古地理[J]. 古地理学报,2008,10(4):341-354. XIAO Jianxin,SUN Fenjin,HE Naixiang,et al. Permian Shanxi Formation and member 8 of Xiashihezi Formation in Ordos Basin:Palaeogeography and catchment area for sediments derived from north and south provenances[J]. Journal of Palaeogeography,2008,10(4):341-354.
[19] 王卫红,田景春,张锦泉. 鄂尔多斯盆地二叠系盒8段沉积特征再研究[J]. 成都理工大学学报(自然科学版),2016,43(2):224-232. WANG Weihong,TIAN Jingchun,ZHANG Jinquan. Research on sedimentary environment of the member8 of Middile Permian Xiashihezi Formation in Ordos Basin,China[J]. Journal of Chengdu University of Technology (Science & Technology Edition),2016,43(2):224-232.
[20] 田景春,吴琦,王峰,等. 鄂尔多斯盆地下石盒子组盒8段储集砂体发育控制因素及沉积模式研究[J]. 岩石学报,2011, 27(8):2403-2412. TIAN Jingchun,WU Qi,WANG Feng,et al. Research on development factors and the deposition model of large area reservoir sandstones of He 8 section of Xiashihezi Formation of Permian in Ordos Basin[J].Acta Petrologica Sinica,2011,27(8):2403-2412.
[21] 于兴河,王德发,郑浚茂. 华北地区二叠系岩相组合类型、剖面特点及沉积体系[J]. 沉积学报,1992,11(1):27-35. YU Xinghe,WANG Defa,ZHENG Junmao. Lithofacies association types or sequences and depositional system of Permian sandstones in north China[J]. Acta Sedimentologica Sinica, 1992,11(1):27-35.
[22] 王德发,郑竣茂,邓宏文. 华北石炭-二叠系古地理沉积环境的初步分析[J]. 地球科学——武汉地质学院学报,1986,11(3):267-272. WANG Defa,ZHENG Junmao,DENG Hongwen. A preliminary analysis of paleogeographic environments in CarboniferousPermian system in northern China[J]. Earth Science-Journal of Wuhan College of Geology,1986,11(3):267-272.
[23] 陈世悦,刘焕杰. 华北地台东部石炭-二叠纪岩相古地理特征[J]. 中国区域地质,1997,16(4):379-386. CHEN Shiyue,LIU Huanjie. Carboniferous-Permian lithofacies and paleogeography in the eastern part of the north China platform[J]. Regional Geology of China,1997,16(4):379-386.
[24] 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. 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.
[1] 关蕴文, 苏思羽, 蒲仁海, 王启超, 闫肃杰, 张仲培, 陈硕, 梁东歌. 鄂尔多斯盆地南部旬宜地区古生界天然气成藏条件及主控因素[J]. 岩性油气藏, 2024, 36(6): 77-88.
[2] 白玉彬, 李梦瑶, 朱涛, 赵靖舟, 任海姣, 吴伟涛, 吴和源. 玛湖凹陷二叠系风城组烃源岩地球化学特征及页岩油“甜点”评价[J]. 岩性油气藏, 2024, 36(6): 110-121.
[3] 王义凤, 田继先, 李剑, 乔桐, 刘成林, 张景坤, 沙威, 沈晓双. 玛湖凹陷西南地区二叠系油气藏相态类型及凝析油气地球化学特征[J]. 岩性油气藏, 2024, 36(6): 149-159.
[4] 魏成林, 张凤奇, 江青春, 鲁雪松, 刘刚, 卫延召, 李树博, 蒋文龙. 准噶尔盆地阜康凹陷东部深层二叠系超压形成机制及演化特征[J]. 岩性油气藏, 2024, 36(5): 167-177.
[5] 杨海波, 冯德浩, 杨小艺, 郭文建, 韩杨, 苏加佳, 杨皩, 刘成林. 准噶尔盆地东道海子凹陷二叠系平地泉组烃源岩特征及热演化史模拟[J]. 岩性油气藏, 2024, 36(5): 156-166.
[6] 尹虎, 屈红军, 孙晓晗, 杨博, 张磊岗, 朱荣幸. 鄂尔多斯盆地东南部三叠系长7油层组深水沉积特征及演化规律[J]. 岩性油气藏, 2024, 36(5): 145-155.
[7] 王子昕, 柳广弟, 袁光杰, 杨恒林, 付利, 王元, 陈刚, 张恒. 鄂尔多斯盆地庆城地区三叠系长7段烃源岩特征及控藏作用[J]. 岩性油气藏, 2024, 36(5): 133-144.
[8] 申有义, 王凯峰, 唐书恒, 张松航, 郗兆栋, 杨晓东. 沁水盆地榆社—武乡区块二叠系煤系页岩储层地质建模及“甜点”预测[J]. 岩性油气藏, 2024, 36(4): 98-108.
[9] 牟蜚声, 尹相东, 胡琮, 张海峰, 陈世加, 代林锋, 陆奕帆. 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.
[10] 徐田录, 吴承美, 张金凤, 曹爱琼, 张腾. 吉木萨尔凹陷二叠系芦草沟组页岩油储层天然裂缝特征与压裂模拟[J]. 岩性油气藏, 2024, 36(4): 35-43.
[11] 孟庆昊, 张昌民, 张祥辉, 朱锐, 向建波. 塔里木盆地现代分支河流体系形态、分布及其主控因素[J]. 岩性油气藏, 2024, 36(4): 44-56.
[12] 冯斌, 黄晓波, 何幼斌, 李华, 罗进雄, 李涛, 周晓光. 渤海湾盆地庙西北地区古近系沙河街组三段源-汇系统重建[J]. 岩性油气藏, 2024, 36(3): 84-95.
[13] 邵威, 周道容, 李建青, 章诚诚, 刘桃. 下扬子逆冲推覆构造后缘凹陷油气富集关键要素及有利勘探方向[J]. 岩性油气藏, 2024, 36(3): 61-71.
[14] 段逸飞, 赵卫卫, 杨天祥, 李富康, 李慧, 王嘉楠, 刘钰晨. 鄂尔多斯盆地延安地区二叠系山西组页岩气源储特征及聚集规律[J]. 岩性油气藏, 2024, 36(3): 72-83.
[15] 曹江骏, 王茜, 王刘伟, 李诚, 石坚, 陈朝兵. 鄂尔多斯盆地合水地区三叠系长7段夹层型页岩油储层特征及主控因素[J]. 岩性油气藏, 2024, 36(3): 158-171.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] 庞雄奇, 陈冬霞, 张　俊. 隐蔽油气藏的概念与分类及其在实际应用中需要注意的问题[J]. 岩性油气藏, 2007, 19(1): 1 -8 .
[2] 雷卞军，张吉，王彩丽，王晓蓉，李世临，刘斌. 高分辨率层序地层对微相和储层的控制作者用——以靖边气田统5井区马五段上部为例[J]. 岩性油气藏, 2008, 20(1): 1 -7 .
[3] 杨杰，卫平生，李相博. 石油地震地质学的基本概念、内容和研究方法[J]. 岩性油气藏, 2010, 22(1): 1 -6 .
[4] 王延奇，胡明毅，刘富艳，王辉，胡治华. 鄂西利川见天坝长兴组海绵礁岩石类型及礁体演化阶段[J]. 岩性油气藏, 2008, 20(3): 44 -48 .
[5] 代黎明, 李建平, 周心怀, 崔忠国, 程建春. 渤海海域新近系浅水三角洲沉积体系分析[J]. 岩性油气藏, 2007, 19(4): 75 -81 .
[6] 段友祥, 曹婧, 孙歧峰. 自适应倾角导向技术在断层识别中的应用[J]. 岩性油气藏, 2017, 29(4): 101 -107 .
[7] 黄龙，田景春，肖玲，王峰. 鄂尔多斯盆地富县地区长6砂岩储层特征及评价[J]. 岩性油气藏, 2008, 20(1): 83 -88 .
[8] 杨仕维，李建明. 震积岩特征综述及地质意义[J]. 岩性油气藏, 2008, 20(1): 89 -94 .
[9] 李传亮，涂兴万. 储层岩石的2种应力敏感机制——应力敏感有利于驱油[J]. 岩性油气藏, 2008, 20(1): 111 -113 .
[10] 李君, 黄志龙, 李佳, 柳波. 松辽盆地东南隆起区长期隆升背景下的油气成藏模式[J]. 岩性油气藏, 2007, 19(1): 57 -61 .

陇ICP备17006252号
版权所有© 2018 中国石油集团西北地质研究所有限公司《岩性油气藏》编辑部

地址：甘肃省兰州市城关区雁儿湾路535号(陇ICP备17006252号)    电话：0931-8686158;8686058;8686288    邮箱：yxyqc@petrochina.com.cn

甘公网安备 62010202002827号

本系统由北京玛格泰克科技发展有限公司设计开发