|本期目录/Table of Contents|

[1]屈雪峰,王武荣,谢启超,等.坳陷湖盆湖底扇储层单砂体构型——以鄂尔多斯盆地合水地区三叠系长6油层组为例[J].地球科学与环境学报,2021,43(05):850-967.[doi:10.19814/j.jese.2020.10041]
 QU Xue-feng,WANG Wu-rong,XIE Qi-chao,et al.Single Sandbody Architecture of Sublacustrine Fan in a Depression Lacustrine Basin—Insights from Triassic Chang-6 Oil-bearing Interval in Heshui Area of Ordos Basin, China[J].Journal of Earth Sciences and Environment,2021,43(05):850-967.[doi:10.19814/j.jese.2020.10041]
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坳陷湖盆湖底扇储层单砂体构型——以鄂尔多斯盆地合水地区三叠系长6油层组为例(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第43卷
期数:
2021年第05期
页码:
850-967
栏目:
基础地质与矿产地质
出版日期:
2021-09-15

文章信息/Info

Title:
Single Sandbody Architecture of Sublacustrine Fan in a Depression Lacustrine Basin—Insights from Triassic Chang-6 Oil-bearing Interval in Heshui Area of Ordos Basin, China
文章编号:
1672-6561(2021)05-0850-18
作者:
屈雪峰1王武荣23谢启超1岳大力23*刘 建1吴胜和23张雪婷23胡嘉靖4
(1. 中国石油长庆油田公司勘探开发研究院,陕西 西安 710018; 2. 中国石油大学(北京)地球科学学院,北京 102249; 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. 中国石油国际勘探开发有限公司,北京 100034)
Author(s):
QU Xue-feng1 WANG Wu-rong23 XIE Qi-chao1 YUE Da-li23* LIU Jian1 WU Sheng-he23 ZHANG Xue-ting23 HU Jia-jing4
(1. Research Institute of Exploration and Development, Changqing Oilfield Company, PetroChina, Xi'an 710018, Shaanxi, China; 2. College of Geosciences, China University of Petroleum, Beijing 102249, China; 3. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China; 4. China National Oil and Gas Exploration and Development Corporation, Beijing 100034, China)
关键词:
湖底扇 单砂体 定量规模 叠置样式 三维构型模式 长6油层组 合水地区 鄂尔多斯盆地
Keywords:
sublacustrine fan single sandbody quantitative scale superimposition pattern three-dimensional architecture model Chang-6 oil-bearing interval Heshui area Ordos Basin
分类号:
P618.13; TE122
DOI:
10.19814/j.jese.2020.10041
文献标志码:
A
摘要:
重力流沉积是目前国际沉积学研究的热点和难点。相比于海底扇储层,湖底扇储层单砂体构型的研究相对薄弱,尤其是定量构型模式研究鲜有报道。综合应用岩芯、测井及生产动态资料,对鄂尔多斯盆地合水地区三叠系长6油层组进行了砂体构型解剖,明确了湖底扇内部单砂体构型特征。结果表明:湖底扇中共识别了6种构型单元类型,即主水道、分支水道、朵叶主体、朵叶侧缘、水道间及朵叶间。基于直井和水平井的单砂体边界识别标志,完成了单砂体边界划分,明确了湖底扇朵叶体由多个单一朵叶体补偿叠置而成,补偿叠置样式受控于短期基准面旋回变化。单一朵叶体在平面上呈舌状,近端略窄,远端略宽,最大宽度与最大厚度之间成明显的线性正相关关系,宽厚比为100~160。基于构型解剖成果,建立了坳陷湖盆湖底扇的三维构型模式。研究成果对油田后期开发方案调整及剩余油分布的挖潜具有重要的指导意义。
Abstract:
The theories involved in gravity flow deposits have become a hot and difficult topic of international sedimentology research. Compared with submarine fan reservoirs, the study on the single sandbody architecture of sublacustrine fan reservoirs is relatively weak, especially the study on quantitative architecture models is still rarely reported. Based on the integrated analysis of the core, well logging and production data, the architectural characteristics of Triassic Chang-6 oil-bearing interval in Heshui area of Ordos Basin were investigated, and the distribution of the single sandbody of sublacustrine fan in depression lacustrine basin was determined. The results show that 6 architecture elements are identified in sublacustrine fan, including main channel, branch channel, lobe, lobe edge, inter-channel and inter-lobe. Based on the single sandbody boundary recognition mark of exploration wells and horizontal wells, the boundary of single sandbody was divided. The lobe complex is composed by multiple individual lobes as the compensational superimposition pattern, which is related to the short-term base-level changing. The single lobe is tongue-shaped on the plane and narrower in the proximal region while wider in the distal region. There is an obvious linear positive correlation between maximum width and maximum thickness, with the aspect ratio ranging from 100 to 160. Finally, according to the analysis results of the architecture in the study area, the three-dimensional architecture model of sublacustrine fan in the depression lacustrine basin is established. The research results have important guiding significance for the adjustment of the oilfield development program and the exploitation of remaining oil.

参考文献/References:

[1] KOLLA V,BOURGES P,URRUTY J M,et al.Evolution of Deep-water Tertiary Sinuous Channels Offshore Angola(West Africa)and Implications for Re-servoir Architecture[J].AAPG Bulletin,2001,85(8):1373-1405.
[2] POSAMENTIER H W,KOLLA V.Seismic Geomorphology and Stratigraphy of Depositional Elements in Deep-water Settings[J].Journal of Sedimentary Research,2003,73(3):367-388.
[3] 庞 雄,陈长民,朱 明,等.深水沉积研究前缘问题[J].地质论评,2007,53(1):36-43.
PANG Xiong,CHEN Chang-min,ZHU Ming,et al.Frontier of the Deep-water Deposition Study[J].Geological Review,2007,53(1):36-43.
[4] 赵俊兴,李凤杰,申晓莉,等.鄂尔多斯盆地南部长6和长7油层浊流事件的沉积特征及发育模式[J].石油学报,2008,29(3):389-394.
ZHAO Jun-xing,LI Feng-jie,SHEN Xiao-li,et al.Sedimentary Characteristics and Development Pattern of Turbidity Event of Chang-6 and Chang-7 Oil Re-servoirs in the Southern Ordos Basin[J].Acta Petrolei Sinica,2008,29(3):389-394.
[5] STEVENSON C J,PEAKALL J.Effects of Topography on Lofting Gravity Flows:Implications for the Deposition of Deep-water Massive Sands[J].Marine and Petroleum Geology,2010,27(7):1366-1378.
[6] WALKER R G.Deep-water Sandstone Facies and An-cient Submarine Fans:Models for Exploration for St-ratigraphic Traps[J].AAPG Bulletin,1978,62(6):932-966.
[7] 刘喜玲,刘君荣.深水沉积及海底扇相模式研究进展[J].长江大学学报(自然科学版),2013,10(14):30-33.
LIU Xi-ling,LIU Jun-rong.Research Progress on Deep-water Deposition and Submarine Fan Facies Model[J].Journal of Yangtze University(Natural Science Edition),2013,10(14):30-33.
[8] NORMARK W R.Growth Patterns of Deep-sea Fans[J].AAPG Bulletin,1970,54(11):2170-2195.
[9] READING H G,RICHARDS M.Turbidite Systems in Deep-water Basin Margins Classified by Grain Size and Feeder System[J].AAPG Bulletin,1994,78(5):213-235.
[10] BROWNE G H,SLATT R M.Outcrop and Behind-outcrop Characterization of a Late Miocene Slope Fan System,Mt.Messenger Formation,New Zealand[J].AAPG Bulletin,2002,86(5):841-862.
[11] GERVAIS A,SAVOYE B,MULDER T,et al.Sandy Modern Turbidite Lobes:A New Insight from High Resolution Seismic Data[J].Marine and Petroleum Geology,2006,23(4):485-502.
[12] 吕 明,王 颖,陈 莹.尼日利亚深水区海底扇沉积模式成因探讨及勘探意义[J].中国海上油气,2008,20(4):275-282.
LU Ming,WANG Ying,CHEN Ying.A Discussion on Original of Submarine Fan Deposition Model and Its Exploration Significance in Nigeria Deep-water Area[J].China Offshore Oil and Gas,2008,20(4):275-282.
[13] 赵晓明,刘 丽,谭程鹏,等.海底水道体系沉积构型样式及控制因素:以尼日尔三角洲盆地陆坡区为例[J].古地理学报,2018,20(5):825-840.
ZHAO Xiao-ming,LIU Li,TAN Cheng-peng,et al.Styles of Submarine-channel Architecture and Its Controlling Factors:A Case Study from the Niger Delta Basin Slope[J].Journal of Palaeogeography,2018,20(5):825-840.
[14] 林 煜,吴胜和,王 星,等.深水浊积朵叶储层构型模式研究[J].天然气地球科学,2014,25(8):1197-1204.
LIN Yu,WU Sheng-he,WANG Xing,et al.Research on Reservoir Architecture Models of Deep-water Turbidite Lobes[J].Natural Gas Geoscience,2014,25(8):1197-1204.
[15] ZHANG J J,WU S H,HU G Y,et al.Sea-level Control on the Submarine Fan Architecture in a Deepwater Sequence of the Niger Delta Basin[J].Marine and Petroleum Geology,2018,94:179-197.
[16] 张佳佳,吴胜和.海底扇朵叶沉积构型研究进展[J].中国海上油气,2019,31(5):88-106.
ZHANG Jia-jia,WU Sheng-he.Research Progress on the Depositional Architecture of Submarine-fan Lobes[J].China Offshore Oil and Gas,2019,31(5):88-106.
[17] 赵澂林,刘孟慧.湖底扇相模式及其在油气预测中的应用[J].华东石油学院学报,1984(4):323-332.
ZHAO Cheng-lin,LIU Meng-hui.Facies Model of Sublacustrine Fan and Its Application in Oil and Gas Prediction[J].Journal of East China Petroleum University,1984(4):323-332.
[18] 刘 芬,朱筱敏,李 洋,等.鄂尔多斯盆地西南部延长组重力流沉积特征及相模式[J].石油勘探与开发,2015,42(5):577-588.
LIU Fen,ZHU Xiao-min,LI Yang,et al.Sedimentary Characteristics and Facies Model of Gravity Flow Deposits of Late Triassic Yanchang Formation in Southwestern Ordos Basin,NW China[J].Petroleum Exploration and Development,2015,42(5):577-588.
[19] MA B B,CAO Y C,ERIKSSON K A,et al.Depositional and Diagenetic Controls on Deeply-buried Eocene Sublacustrine Fan Reservoirs in the Dongying Depression,Bohai Bay Basin,China[J].Marine and Petroleum Geology,2017,82:297-317.
[20] ZOU C N,WANG L,LI Y,et al.Deep-lacustrine Transformation of Sandy Debrites into Turbidites,Upper Triassic,Central China[J].Sedimentary Geology,2012,265/266:143-155.
[21] 张庆石,张 革,陈彬滔,等.松辽盆地坳陷期湖底扇沉积特征与分布规律:以英台地区青山口组为例[J].天然气地球科学,2014,25(3):318-325.
ZHANG Qing-shi,ZHANG Ge,CHEN Bin-tao,et al.Deposition Characteristics and Distribution Pattern of Sublacustrine Fan in Qingshankou Formation,Song-liao Basin[J].Natural Gas Geoscience,2014,25(3):318-325.
[22] YANG T,CAO Y C,FRIIS H,et al.Genesis and Distribution Pattern of Carbonate Cements in Lacustrine Deep-water Gravity-flow Sandstone Reservoirs in the Third Member of the Shahejie Formation in the Dongying Sag,Jiyang Depression,Eastern China[J].Marine and Petroleum Geology,2018,92:547-564.
[23] 德勒恰提·加娜塔依,张明玉,陈春勇,等.准噶尔盆地吉木萨尔凹陷东部二叠系梧桐沟组湖底扇沉积特征及展布[J].石油学报,2015,36(6):688-698.
DELEQIAT Janney,ZHANG Ming-yu,CHEN Chun-yong,et al.Sedimentary Characteristics and Distribution of Sublacustrine Fan in Permian Wutonggou Formation,Eastern Jimsar Sag,Junggar Basin[J].Acta Petrolei Sinica,2015,36(6):688-698.
[24] 吴 冬,朱筱敏,马爱钰,等.鄂尔多斯盆地合水—塔尔湾地区长6~长10油层组沉积相研究[J].中国地质,2015,42(6):1822-1836.
WU Dong,ZHU Xiao-min,MA Ai-yu,et al.Sedimentary Facies of the Chang-6-Chang-10 Intervals in He-shui-Ta'erwan Area,Ordos Basin[J].Geology in China,2015,42(6):1822-1836.
[25] 王文枫,岳大力,赵继勇,等.利用地震正演模拟方法研究地层结构:以鄂尔多斯盆地合水地区延长组三段为例[J].石油地球物理勘探,2020,55(2):411-418.
WANG Wen-feng,YUE Da-li,ZHAO Ji-yong,et al.Research on Stratigraphic Structure Based on Seismic Forward Modeling:A Case Study of the Third Member of the Yanchang Formation in Heshui Area,Ordos Basin[J].Oil Geophysical Prospecting,2020,55(2):411-418.
[26] WANG W R,YUE D L,ZHAO J Y,et al.Diagenetic Alteration and Its Control on Reservoir Quality of Tight Sandstones in Lacustrine Deep-water Gravity-flow Deposits:A Case Study of the Yanchang Formation,Southern Ordos Basin,China[J].Marine and Petroleum Geology,2019,110:676-694.
[27] WANG W R,YUE D L,KENNETH A E,et al.Quantification and Prediction of Pore Structures in Tight Oil Reservoirs Based on Multifractal Dimensions from Integrated Pressure- and Rate-controlled Porosimetry for the Upper Triassic Yanchang Formation,Ordos Basin,China[J].Energy and Fuels,2020,34(4):4366-4383.
[28] 刘九洲,张春生,狄贵东,等.鄂尔多斯盆地华庆地区长63油层沉积相研究[J].特种油气藏,2010,17(5):57-59.
LIU Jiu-zhou,ZHANG Chun-sheng,DI Gui-dong,et al.Sedimentary Facies of the Chang-63 Reservoir in the Huaqing Area of the Ordos Basin[J].Special Oil and Gas Reservoirs,2010,17(5):57-59.
[29] 夏青松,田景春.鄂尔多斯盆地西南部上三叠统长6油层组湖底扇特征[J].古地理学报,2007,9(1):33-43.
XIA Qing-song,TIAN Jing-chun.Sedimentary Cha-racteristics of Sublacustrine Fan of the Interval 6 of Yanchang Formation of Upper Triassic in South-western Ordos Basin[J].Journal of Palaeogeography,2007,9(1):33-43.
[30] LIU J P,XIAN B Z,WANG J H,et al.Sedimentary Architecture of a Sub-lacustrine Debris Fan:Eocene Dongying Depression,Bohai Bay Basin,East China[J].Sedimentary Geology,2017,362:66-82.
[31] 杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京:石油工业出版社,2002.
YANG Jun-jie.Tectonic Evolution and Oil-gas Distribution Rules in Ordos Basin[M].Beijing:Petroleum Industry Press,2002.
[32] 付金华,邓秀芹,楚美娟,等.鄂尔多斯盆地延长组深水岩相发育特征及其石油地质意义[J].沉积学报,2013,31(5):928-938.
FU Jin-hua,DENG Xiu-qin,CHU Mei-juan,et al.Features of Deepwater Lithofacies,Yanchang Formation in Ordos Basin and Its Petroleum Significance[J].Acta Sedimentologica Sinica,2013,31(5):928-938.
[33] 姚泾利,赵彦德,刘广林,等.鄂尔多斯盆地三叠系长9段多源成藏模式[J].石油勘探与开发,2018,45(3):373-384.
YAO Jing-li,ZHAO Yan-de,LIU Guang-lin,et al.Formation Patterns of Chang-9 Oil Reservoir in Triassic Yanchang Formation,Ordos Basin,NW China[J].Petroleum Exploration and Development,2018,45(3):373-384.
[34] 姚泾利,曾溅辉,罗安湘,等.致密储层源储结构对储层含油性的控制作用——以鄂尔多斯盆地合水地区长6~长8段为例[J].地球科学与环境学报,2019,41(3):267-280.
YAO Jing-li,ZENG Jian-hui,LUO An-xiang,et al.Controlling Effect of Source-reservoir Structure in Tight Reservoir on Oil-bearing Property—A Case Study of Chang-6-Chang-8 Members in Heshui Area of Ordos Basin,China[J].Journal of Earth Sciences and Environment,2019,41(3):267-280.
[35] 杨 华,邓秀芹.构造事件对鄂尔多斯盆地延长组深水砂岩沉积的影响[J].石油勘探与开发,2013,40(5):513-520.
YANG Hua,DENG Xiu-qin.Deposition of Yanchang Formation Deep-water Sandstone Under the Control of Tectonic Events,Ordos Basin[J].Petroleum Exploration and Development,2013,40(5):513-520.
[36] 崔龙涛,郝 帅,王春平,等.鄂尔多斯盆地镇原北部三叠系延长组长7—长6油层组古地貌与砂体分布特征[J].古地理学报,2015,17(6):805-812.
CUI Long-tao,HAO Shuai,WANG Chun-ping,et al.Palaeogeomorphology Reconstruction and Sandbody Distribution of the Chang-7-Chang-6 Intervals of Triassic Yanchang Formation in Northern Zhenyuan Area,Ordos Basin[J].Journal of Palaeogeography,2015,17(6):805-812.
[37] 付金华,邓秀芹,张晓磊,等.鄂尔多斯盆地三叠系延长组深水砂岩与致密油的关系[J].古地理学报,2013,15(5):624-634.
FU Jin-hua,DENG Xiu-qin,ZHANG Xiao-lei,et al.Relationship Between Deepwater Sandstone and Tight Oil of the Triassic Yanchang Formation in Ordos Basin[J].Journal of Palaeogeography,2013,15(5):624-634.
[38] 杨 华,刘自亮,朱筱敏,等.鄂尔多斯盆地西南缘上三叠统延长组物源与沉积体系特征[J].地学前缘,2013,20(2):10-18.
YANG Hua,LIU Zi-liang,ZHU Xiao-min,et al.Pro-venance and Depositional Systems of the Upper Triassic Yanchang Formation in the Southwestern Ordos Basin,China[J].Earth Science Frontiers,2013,20(2):10-18.
[39] 曹江骏,杨友运,陈朝兵,等.致密砂岩储层骨架砂体构型特征:以鄂尔多斯盆地合水地区延长组长6段砂体为例[J].沉积学报,2019,37(6):1103-1116.
CAO Jiang-jun,YANG You-yun,CHEN Chao-bing,et al.Analysis of Configuration Characteristics for Skeleton Sand Body with Tight Sandstone Reservoir:A Case Study of Triassic Chang-6 Members in Heshui Area,Ordos Basin,NW China[J].Acta Sedimentolo-gica Sinica,2019,37(6):1103-1116.
[40] 惠 潇,张海峰.鄂尔多斯盆地延长组长6期湖盆中部砂体发育特征[J].地球科学与环境学报,2009,31(1):53-57.
HUI Xiao,ZHANG Hai-feng.Characters of Sand Bo-dies in Chang-6 Section of Yanchang Formation in the Central Lake Basin of Ordos Basin[J].Journal of Earth Sciences and Environment,2009,31(1):53-57.
[41] LI X B,LIU H Q,PAN S X,et al.Subaqueous Sandy Mass-transport Deposits in Lacustrine Facies of the Upper Triassic Yanchang Formation,Ordos Basin,Central China[J].Marine and Petroleum Geology,2018,97:66-77.
[42] 吴胜和,纪友亮,岳大力,等.碎屑沉积地质体构型分级方案探讨[J].高校地质学报,2013,19(1):12-22.
WU Sheng-he,JI You-liang,YUE Da-li,et al.Discussion on Hierarchical Scheme of Architectural Units in Clastic Deposits[J].Geological Journal of China Universities,2013,19(1):12-22.
[43] 岳大力,吴胜和,谭河清,等.曲流河古河道储层构型精细解剖:以孤东油田七区西馆陶组为例[J].地学前缘,2008,15(1):101-109.
YUE Da-li,WU Sheng-he,TAN He-qing,et al.An Anatomy of Paleochannel Reservoir Architecture of Meandering River Reservoir:A Case Study of Guantao Formation,the West 7th Block of Gudong Oilfield[J].Earth Science Frontiers,2008,15(1):101-109.
[44] 岳大力,吴胜和,刘建民.曲流河点坝地下储层构型精细解剖方法[J].石油学报,2007,28(4):99-103.
YUE Da-li,WU Sheng-he,LIU Jian-min.An Accurate Method for Anatomizing Architecture of Subsurface Reservoir in Point Bar of Meandering River[J].Acta Petrolei Sinica,2007,28(4):99-103.
[45] 罗 可.东辛油田营17断块沙二段沉积特征研究[D].青岛:中国石油大学,2017.
LUO Ke.Sedimentary Characteristics of the Second Member of the Shahejie Formation in the Ying-17 Fault Block from Dongxin Oilfield[D].Qingdao:China University of Petroleum,2017.
[46] 张佳佳.西非OML130区块海底扇朵叶体系构型模式研究[D].北京:中国石油大学,2012.
ZHANG Jia-jia.Research on the Architecture Model of Submarine Lobe System:A Case Study of OML130 Block Offshore,West Africa[J].Beijing:China University of Petroleum,2012.

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备注/Memo

备注/Memo:
收稿日期:2020-10-30; 修回日期:2021-02-04投稿网址:http:∥jese.chd.edu.cn/
基金项目:中国石油天然气集团有限公司-中国石油大学(北京)战略合作科技专项项目(ZLZX2020-02); 国家科技重大专项项目(2017ZX05013002-004); 中国石油天然气股份有限公司重大科技专项项目(2016E-0505)
作者简介:屈雪峰(1972-),女,山西运城人,教授级高级工程师,E-mail:qxf_cq@petrochina.com.cn。
*通讯作者:岳大力(1974-),男,黑龙江巴彦人,教授,博士研究生导师,理学博士,E-mail:yuedali@cup.edu.cn。
更新日期/Last Update: 2021-09-30