松辽盆地南部东南隆起区白垩系登娄库组沉积特征

doi:10.11743/ogg20140315

石油与天然气地质 ›› 2014, Vol. 35 ›› Issue (3): 401-409.doi: 10.11743/ogg20140315

松辽盆地南部东南隆起区白垩系登娄库组沉积特征

李占东¹, 李阳², 刘云利³, 胡慧婷⁴, 马凤荣⁴, 张小刚⁵

1. 东北石油大学石油工程学院, 黑龙江大庆, 163318;
2. 大庆职业学院, 黑龙江大庆, 163255;
3. 中国石油新疆油田分公司风城油田作业区, 新疆克拉玛依 834000;
4. 东北石油大学地球科学学院, 黑龙江大庆, 163318;
5. 中国石油长庆油田分公司勘探部, 陕西西安, 710018

收稿日期:2013-09-25 修回日期:2014-01-28 出版日期:2014-06-08 发布日期:2014-07-11
通讯作者: 李阳（1985- ），女，讲师，油藏地质。E-mail：249562496@qq.com。 E-mail:249562496@qq.com
第一作者简介:李占东（1979- ），男，博士、副教授，油藏描述和油田开发。E-mail：conquereast@163.com。
基金项目:
国家高技术研究发展计划（863计划）项目（SS2012AA060203）。

Sedimentary characteristics of the Cretaceous Denglouku Formation in the southeast uplift of the southern Songliao Basin

Li Zhandong¹, Li Yang², Liu Yunli³, Hu Huiting⁴, Ma Fengrong⁴, Zhang Xiaogang⁵

1. College of Petroleum Engineering Institute, Northeast Petroleum University, Daqing, Heilongjiang 163318, China;
2. Daqing Vocational College, Daqing, Heilongjiang 163255, China;
3. Fengcheng Oilfield Operation Area, PetroChina Xinjiang Oilfield Company, Karamay, Xinjiang 834000, China;
4. College of Earth Sciences, Northeast Petroleum University, Daqing, Heilongjiang PetroChina, 163318, China;
5. Exploration Department of Changqing Oilfield Company, PetroChina, Xi'an, Shanxi 710018, China

Received:2013-09-25 Revised:2014-01-28 Online:2014-06-08 Published:2014-07-11

摘要/Abstract

摘要：

为了查明松辽盆地南部东南隆起区登娄库组沉积特征及演化规律，开展了层序格架内的沉积相展布特征及演化研究。研究表明，登娄库组物源具有四周向中央汇聚的继承性特征，沉积相分布受盆地构造演化控制明显，主要发育了5种沉积相——冲积扇、扇三角洲、辫状河、辫状河三角洲和湖相。层序Ⅳ-d1为断-坳转换期的早期，沉积受断陷控制明显，致使沉积物快速卸载，各沉积体系向盆地内部进积的距离受到了限制，共发育了5个规模较大的分割式断陷和2个小型断陷。断陷周缘古凸起为冲积扇沉积体系的主要发育区，扇三角洲沉积分布于断陷的四周，扇三角洲前缘延伸到入湖处。沉积相主要以冲积扇、扇三角洲和湖相为主；层序Ⅳ-d2为断坳转换期的末期，研究区基本上形成了统一沉积物卸载区域，湖泊范围扩大，主要发育了冲积扇、扇三角洲、辫状河、辫状河三角洲和湖相沉积。以泛滥平原与滨浅湖的接触带为界，该界限以西主要发育来自西部和北部物源高地的冲积扇、辫状河沉积体系，该界限以东湖泊相大面积发育，伴随高地物源区碎屑沉积物陆续注入湖盆，构成了规模不等的退积式扇三角洲。其中，扇三角洲前缘和辫状河三角洲前缘亚相带是油气富集的主要储集体，是今后该区登娄库组油气勘探的有利相带。

关键词: 沉积相, 登娄库组, 白垩系, 松辽盆地东南隆起区

Abstract:

Sedimentary characteristics and evolution of the Denglouku Formation in the southeast uplift area of southern Songliao basin was studied based on analyses of sedimentary facies distribution and evolution in the context of sequence framework.The results show that the provenance of the Formation were distributed around the basin and supplied sediments from all directions to the center of the basin and the sedimentary facies distribution was controlled by basin tectonic evolution.Five major sedimentary facies were recognized in the area:alluvial fan,fan delta,braided river,braided delta,and lake.The sequence Ⅳ-d1 was formed during the early stage of transformation from a fault depression to a sag.The deposition was mostly controlled by the fault depression and the sediments were downloaded rapidly,restricting the distance of progradation to the inner basin.There developed five separated fault depressions and two small fault depression.Alluvial fan sedimentary systems were developed on the paleohighs around the fault depressions,fan delta systems were located around the fault depressions,while the fronts of the fan delta extended into the mouth of the lake.The sedimentary facies were dominated by alluvial fan,fan delta and lake.Sequence Ⅳ-d2 was formed during the late stage of transformation from fault depression to a sag when an unified sediment unloading area was developed,and the lake expanded.The sedimentary facies were dominated by alluvial fan,fan delta,braided river,braided river delta,littoral and lake.The contact zone of the flood plains and the shore-shallow lake can be regarded as a boundary,to the west of which formed allu-vial fan and braided river systems with sediments sourced from the western and the northern highland provenances;and to the east of which developed retrograded fan deltas of different scales with clastic sediments sourced from highlands.Among the facies,the fan delta front and braided river delta front are considered to be home to hydrocarbon reservoirs and therefore are the most promising exploration targets for oil and gas.

Key words: sedimentary facies, Denglouku Formation, Cretaceous, southeast uplift of the Songliao Basin

中图分类号:

TE121.3

李占东,李阳,刘云利,等. 松辽盆地南部东南隆起区白垩系登娄库组沉积特征[J]. 石油与天然气地质, 2014, 35(3): 401-409. doi: 10.11743/ogg20140315 Li Zhandong,Li Yang,Liu Yunli,et al. Sedimentary characteristics of the Cretaceous Denglouku Formation in the southeast uplift of the southern Songliao Basin[J]. Oil & Gas Geology, 2014, 35(3): 401-409. doi: 10.11743/ogg20140315

参考文献

[1] 李君,黄志龙,李凌君,等.对松辽盆地南部东南隆起区抬升过程的新认识[J].新疆石油地质,2008,29(6):690-692. Li Jun,Huang Zhilong,Li Lingjun,et al.New understanding of uplifting process of southeast uplift area in southern Songliao Basin[J].Xinjiang Petroleum Geology,2008,29(6):690-692.
[2] 高有峰,王璞珺,瞿雪娇,等.松辽盆地东南隆起区白垩系嫩江组一段沉积相、旋回及其与松科1井的对比[J].岩石学报,2010,26(1):99-108. Gao Youfeng,Wang Pujun,Qu Xuejiao,et al.Sedimentary facies and cyclostratigraphy of the Cretaceous first member of Nenjiang Formation in the southeast uplift zone,Songliao Basin and its correlation with the CCSD-SK-I[J].Acta Petrological Sinica,2010,26(1):99-108.
[3] 程日辉,王国栋,王璞珺.松辽盆地白垩系泉三段-嫩江组沉积旋回与米兰科维奇周期[J].地质学报,2008,82(1):55-64. Cheng Rihui,Wang Guodong,Wang Pujun.Sedimentary cycles of the Cretaceous Quantou-Nenjing Formation and Milankovitch cycles of the South Hole of the SLCORE-Ⅰ in the Songliao Basin[J].Acta Geologica Sinica,2008,82(1):55-64.
[4] 庞智英,舒萍,纪学雁,等.松辽盆地东南隆起区白垩系营城组二段沉积相分析及层序划分[J].吉林大学学报(地球科学版),2009,39(2):232-237. Pang Zhiying,Shu Ping,Ji Xueyan,et al.Sedimentary facies analysis and stratigraphic sequence division of the second member of the Yingcheng Formation in the southeastern uplift region,Songliao Basin[J].Journal of Jilin University(Earth Science Edition),2009,39(2):232-237.
[5] 刘万洙,邵锐,白雪峰,等.松辽盆地东南隆起区营城组一段熔浆胶结复成分砾岩特征及其成因分析[J].吉林大学学报(地球科学版),2007,37(6):1124-1130. Liu Wanzhu,Shao Rui,Bai Xuefeng,et al.Characteristics and genetical study of the magma-cemented polymictic conglomerate in the Cretaceous Yingcheng Formation,southeastern uplift area of the Songliao Basin[J].Journal of Jilin University(Earth Science Edition),2007,37(6):1124-1130.
[6] 叶德燎.松辽盆地东南隆起区下白垩统层序地层格架及油气成藏规律[J].地质科学,2005,40(2):227-236. Ye Deliao.Lower Cretaceous sequence stratigraphic framework and hydrocarbon accumulation in the southeast rise,Songliao Basin,China[J].Chinese Journal of Geology,2005,40(2):227-236.
[7] 李君,黄志龙,李佳,等.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. Li Jun,Huang Zhilong,Li Jia,et al.The pool-forming pattern in the condition of arching in the southeast uplift in Songliao Basin[J].Lithologic Reservoirs,2007,19(1):57-61.
[8] 王宗礼,李君,林世国,等.松辽盆地南部东南隆起区低压油气藏形成机制及分布特征研究[J].天然气地球科学,2009,20(2):216-221. Wang Zongli,Li Jun,Lin Shiguo,et al.Forming mechanism and distribution of low pressure reservoirs in southeast uplift of southern Songliao Basin[J].Natural Gas Geoscience,2009,20(2):216-221.
[9] 李占东,赵伟,李阳,等.开发地震反演可行性研究及应用——以大庆长垣北部油田为例[J].石油与天然气地质,2011,54(32):797-806. Li Zhandong,Zhao Wei,Li Yang,et al.Feasibility study and application of development seismic inversion——a case study from northern Changyuan oilfield of Daqing area[J].Oil & Gas Geology,2011,54(32):797-806.
[10] 国景星,戴启德,吴丽艳,等.冲积河流相层序地层学研究[J].中国石油大学学报(自然科学版),2003,27(4):15-19. Guo Jingxing,Dai Qide,Wu Liyan,et al.Study on alluvial-fluvial facies sequence stratigraphy[J].Journal of China University of Petroleum Edition of Natural Science,2003,27(4):15-19.
[11] 刘忠宝,杨圣彬,焦存礼,等.塔里木盆地巴楚隆起中、下寒武统高精度层序地层与沉积特征[J].石油与天然气地质,2012,33(1):70-76. Liu Zhongbao,Yang Shengbin,Jiao Cunli,et al.High resolution sequence stratigraphy and sedimentary characteristics of the Middle-Lower Cambrian in Bachu Uplift,the Tarim Basin[J].Oil & Gas Geo-logy,2012,33(1):70-76.
[12] 纪友亮,蒙启安,单敬福,等.塔南-南贝尔凹陷南屯组下部沉积体系平面展布特征[J].石油实验地质,2011,33(3):260-265. Ji Youliang,Meng Qi'an,Shan Jingfu,et al.Depositional system of lower Nantun Formation in South Tamuchage-South Beier Sag[J].Petroleum Geology & Experiment,2011,33(3):260-265.
[13] 远光辉,操应长,王艳忠.东营凹陷民丰地区沙河街组四段—三段中亚段沉积相与沉积演化特征[J].石油与天然气地质,2012,33(2):277-286. Yuan Guanghui,Cao Yingchang,Wang Yanzhong.Sedimentary facies and their evolution of the 4th-middle 3rd members of Shahejie Formation in Minfeng area,Dongying Sag[J].Oil & Gas Geology,2012,33(2):277-286.
[14] Holmes A.Principles of physical geology[M].London:Edinburgh,1965:730.
[15] 莫午零,吴朝东,张顺,等.松辽盆地北部上白垩统嫩江组物源及古流向分析[J].石油实验地质,2012,34(1):40-46. Mo Wuling,Wu Chaodong,Zhang Shun,et al.Provenance and palaeo-current direction of Upper Cretaceous Nenjiang Formation in northern Songliao Basin[J].Petroleum Geology & Experiment,2012,34(1):40-46.
[16] Walker R G.Deep-water sandstone facies and ancient submarine fans:models for exploration for stratigraphic traps[J].AAPG Bulletin,1978,62(6):932-966.
[17] 杨勇强,邱隆伟,李聪,等.不同类型盆缘区沉积体系展布与演化——以东营凹陷南坡博东潜山周缘地区为例[J].石油实验地质,2012,34(6):604-610. Yang Yongqiang,Qiu Longwei,Li Cong,et al.Distribution and evolution of sedimentary system in different types of basin edge:a case study of peripheral regions of Bodong Buried Hill,Dongying Sag[J].Petroleum Geology & Experiment,2012,34(6):604-610.
[18] 罗佳强,任延广,吴朝东,等.松辽盆地徐家围子断陷营四段沉积相研究[J].石油实验地质,2010,32(2):140-146. Luo Jiaqiang,Ren Yanguang,Wu Chaodong,et al.Research of sedimentary facies of fourth member of Yingcheng Formation in Xujiaweizi Fault Depression in the Songliao Basin[J].Petroleum Geology & Experiment,2010,32(2):140-146.
[19] McPherson J G.,Shanmugam G,Moiola R J.Fan-deltas and braid-deltas:varieties of coarse-grained deltas[J].Geological Society of America Bulletin,1987,99(3):331-340.
[20] 焦里力,俞昊,任涛.长岭凹陷腰英台油田腰西区块青山口组储层沉积微相研究[J].石油实验地质,2011,33(3):249-254. Jiao Lili,Yu Hao,Ren Tao.Sedimentary microfacies of Qingshankou Formaiton,West-Yao Block,Yaoyingtai oil field,Changling Sag,Songliao Basin[J].Petroleum Geology & Experiment,2011,33(3):249-254.
[21] 魏祥峰,张廷山,梁兴,等.海安凹陷曲塘、海北次凹戴南组—三垛组一段沉积特征及演化[J].石油与天然气地质,2012,33(2):265-276. Wei Xiangfeng,Zhang Tingshan,Liang Xing,et al.Sedimentary cha-racteristics and evolution of the 1st member of Dainan Formation and the 1^st member of Sanduo Formation in Qutang and Haibei Sub-sags,Hai'an Sag[J].Oil & Gas Geology,2012,33(2):265-276.
[22] 李占东,卢双舫,李军辉,等.松辽盆地肇源—太平川地区白垩系姚家组一段沉积特征及演化[J].中南大学学报(自然科学版),2011,42(12):3818-3825. Li Zhandong,Lu Shuangfang,Li Junhui,et al.Sedimentary characteristics and evolution of member 1 Yaojia Formation of Cretaceous in Zhaoyuan-Taipingchuan area of Songliao Basin[J].Journal of Central South University(Science and Technology),2011,42(12):3818-3825.
[23] Maill A D.Reservoir heterogeneities in fluvial sandstones:lesson from outcrop studies[J].AAPG Bulletin,1988,72(6):682-697.
[24] 江青春,王海,李丹,等.地震波形分类技术应用条件及其在葡北地区沉积微相研究中的应用[J].石油与天然气地质,2012,33(1):135-140. Jiang Qingchun,Wang Hai,Li Dan,et al.Application conditions of seismic waveform classification technique and its use in the study of sedimentary microfacies of Pubei area[J].Oil & Gas Geology,2012,33(1):135-140.
[25] 李建青,蒲仁海,武岳,等.江苏黄桥地区龙潭组沉积相与有利储层预测[J].石油实验地质,2012,34(4):395-399. Li Jianqing,Pu Renhai,Wu Yue,et al.Sedimentary characteristics and favorable reservoir prediction of Longtan Formation in Huangqiao area,Jiangsu Province[J].Petroleum Geology & Experiment,2012,34(4):395-399.
[26] 刘双莲,李浩,周小鹰.大牛地气田大12—大66井区沉积微相与储层产能关系[J].石油与天然气地质,2012,33(1):45-49. Liu Shuanglian,Li Hao,Zhou Xiaoying.Relationship between sedimentary microfacies and reservoir productivity in Da12-Da66 wellblock,Daniudi gas field[J].Oil & Gas Geology,2012,33(1):45-49.
[27] 闵小刚,陈开远,范廷恩.井-震结合进行河流相储层非均质性表征——以渤海湾盆地黄河口凹陷渤中263油田为例[J].石油与天然气地质,2011,31(3):375-381. Min Xiaogang,Chen Kaiyuan,Fan Ting'en.Heterogeneity characte-rization of fluvial facies reservoirs through integration of seismic and logging data:an example from Bozhong-263 oilfield in the Huanghekou Sag,Bohai Bay Basin[J].Oil & Gas Geology,2011,31(3):375-381.
[28] 李占东,李阳,张海翔,等.海拉尔盆地乌尔逊—贝尔凹陷大磨拐河组油气成藏条件[J].石油实验地质,2011,33(5):480-487. Li zhandong,Li Yang,Zhang Haixiang,et al.Petroleum accumulation conditions of Damoguaihe Formation in Urxun-Beier Sag,Hailaer Basin[J].Petroleum Geology & Experiment,2011,33(5):480-487.
[29] 赵波,冯子辉,梁江平.松辽盆地安达地区泉头组四段沉积特征与油气分布关系[J].石油实验地质,2010,32(1):35-40. Zhao Bo,Feng Zihui,Liang Jiangping.Sedimentary characteristics and oil and gas distribution in member 4 of Quantou Formation,Anda area,Songliao Basin[J].Petroleum Geology & Experiment,2010,32(1):35-40.

松辽盆地南部东南隆起区白垩系登娄库组沉积特征

Sedimentary characteristics of the Cretaceous Denglouku Formation in the southeast uplift of the southern Songliao Basin

PDF (PC)

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

[1]	潘虹, 于庆森, 李晓山, 宋俊强, 蒋志斌, 王丽, 罗官幸, 徐文秀, 尤浩宇. 准噶尔盆地红车断裂带石炭系重新认识及油气成藏特征[J]. 石油与天然气地质, 2024, 45(1): 215-230.
[2]	侯读杰, 吴克强, 尤丽, 张自鸣, 李雅君, 熊小峰, 徐敏, 严夏泽, 陈威合, 程熊. 琼东南盆地陆源海相烃源岩有机质富集机理[J]. 石油与天然气地质, 2024, 45(1): 31-43.
[3]	屈海洲, 郭新宇, 徐伟, 李文皓, 唐松, 邓雅霓, 何仕鹏, 张云峰, 张兴宇. 碳酸盐岩微孔隙的分类、成因及对岩石物理性质的影响[J]. 石油与天然气地质, 2023, 44(5): 1102-1117.
[4]	高志勇, 吴永平, 刘兆龙, 魏聪, 张永忠, 王翠丽, 刘群明. 塔里木盆地库车坳陷中秋1井区白垩系巴什基奇克组砂质辫状河有利岩相组合发育模式与意义[J]. 石油与天然气地质, 2023, 44(5): 1141-1158.
[5]	李东伟, 龚承林, 胡林, 何小胡, 罗泉源. 深水水道沉积内幕级次划分与精细刻画[J]. 石油与天然气地质, 2023, 44(3): 553-564.
[6]	郑和荣, 田景春, 胡宗全, 张翔, 赵永强, 孟万斌. 塔里木盆地奥陶系岩相古地理演化及沉积模式[J]. 石油与天然气地质, 2022, 43(4): 733-745.
[7]	王胜军, 唐永亮, 朱松柏, 谢伟, 单长安, 聂延波, 王勇, 王益民, 蒋国军, 邵剑波, 叶璁琛. 塔里木盆地库车坳陷北部典型露头剖面白垩系巴什基奇克组三段高分辨率层序地层特征[J]. 石油与天然气地质, 2022, 43(4): 804-822.
[8]	刘晓宁, 姜在兴, 袁晓冬, 陈晨, 王成. 滦平盆地白垩系细粒火山物质对页岩油气形成的影响[J]. 石油与天然气地质, 2022, 43(2): 390-406.
[9]	毛先宇, 宋本彪, 韩如冰, 田昌炳, 李保柱, 宋海强. 伊拉克南部白垩系Mishrif组碳酸盐缓坡潮道沉积特征[J]. 石油与天然气地质, 2020, 41(6): 1233-1243, 1256.
[10]	宫越, 冯志强, 邬长武, 田纳新, 马天碧, 王大鹏, 陶崇智, 高蔚原. 西非北部塞内加尔盆地白垩系陆源碎屑沉积体系及其控制因素[J]. 石油与天然气地质, 2020, 41(6): 1244-1256.
[11]	贺婷婷, 段太忠, 赵磊, 刘彦锋. 塔里木盆地塔河油田T区三叠纪沉积模式[J]. 石油与天然气地质, 2019, 40(4): 822-834.
[12]	刘可禹, 刘畅. “化学-沉积相”分析：一种研究细粒沉积岩的有效方法[J]. 石油与天然气地质, 2019, 40(3): 491-503.
[13]	王亚, 杨少春, 路研, 马宝全, 赵永福, 王永超. 渤海湾盆地东营凹陷高青地区中生界低渗透碎屑岩有效储层特征及发育控制因素[J]. 石油与天然气地质, 2019, 40(2): 271-283.
[14]	黎荣, 胡明毅, 杨威, 刘满仓. 四川盆地中二叠统沉积相模式及有利储集体分布[J]. 石油与天然气地质, 2019, 40(2): 369-379.
[15]	王延章, 林红梅, 冯建伟, 栗宝鹃, 曹晓莉, 蔡宏兴, 胡秋媛. 砂砾岩物源供给能力定量评价——以济阳坳陷车镇凹陷郭局子洼陷为例[J]. 石油与天然气地质, 2018, 39(6): 1154-1163.