吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (1): 31-40.doi: 10.13278/j.cnki.jjuese.20180275

• 地质与资源 • 上一篇    

末端扇—滨浅湖滩坝组合沉积机制与演化分布:以东濮凹陷卫城油田沙河街组四段为例

李维禄1, 高思宇1, 张翼2, 张金亮3, 韩春花1   

  1. 1. 国家海洋信息中心, 天津 300171;
    2. 江苏省地质勘查技术研究院, 南京 210049;
    3. 北京师范大学地理科学学部, 北京 100875
  • 收稿日期:2018-10-27 发布日期:2020-02-11
  • 作者简介:李维禄(1987-),男,助理研究员,主要从事油气田开发地质与矿产资源评价相关方向的研究,E-mail:qrange@163.com
  • 基金资助:
    国家自然科学基金项目(41172109);山东省自然科学基金项目(ZR2011DM009)

Sedimentary Mechanism, Evolution and Distribution of Terminal Fan to Beach-Bar in Shore-Shallow Lake Sediments: A Case Study of 4th Member of Shahejie Formation in Weicheng Oildfield, Dongpu Depression

Li Weilu1, Gao Siyu1, Zhang Yi2, Zhang Jinliang3, Han Chunhua1   

  1. 1. National Marine Data and Information Service, Tianjin 300171, China;
    2. Geological Exploration Technology Institute of Jiangsu Province, Nanjing 210049, China;
    3. Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
  • Received:2018-10-27 Published:2020-02-11
  • Supported by:
    Supported by National Natural Science Foundation of China (41172109) and Natural Science Foundation of Shandong Province (ZR2011DM009)

摘要: 复杂沉积环境下沉积相及其演化的准确描述可以有效地指导油气田的勘探和开发过程。结合东濮凹陷卫城油田的区域沉积背景,利用岩心描述、录测井和分析测试等资料对东濮凹陷卫城油田卫81区块沙河街组四段的沉积特征与沉积相模式进行了全面分析。结果显示:该区块地层发育末端扇-滨浅湖滩坝相过渡型沉积,沙四下段河流末端能量损失、流量波动,发育末端扇沉积,分流河道顺物源方向向河道漫溢和泥滩演化,形成扇状堆积体;随湖平面频繁大面积扩张收缩等沉积环境变化,沙四上段演化为滨浅湖滩坝沉积,滩坝砂体整体呈复合砂体连片平行于主控断层走向分布。

关键词: 末端扇—滨浅湖滩坝组合沉积, 沉积模式, 沉积演化, 砂体分布, 卫城油田, 东濮凹陷

Abstract: The accurate description to sedimentary facies and its evolution of the complicated depositional environment can effectively guide the oil and gas field exploration and exploitation. Combined with the regional background of Weicheng structure in Dongpu depression, the depositional features and sedimentary model of the 4th member of Shahejie Formation (Es4) in Wei 81 block of Weicheng oildfield were analyzed by use of the data of core description, logging, analysis and test, etc. It is considered that the associated sediments of terminal fan to beach-bar in shore-shallow lake are developed in the study formation of this block. The terminal fan was developed in the background of energy loss and flow fluctuation at the end of the rivers in the lower part of Es4, and the distributary channel evolved into overflow or mudflat along the source direction,thus forming the fan-shape accumulation; with the change of sedimentary environment under the frequent expansion or shrink of the lake level, the beach-bar sediments in shore-shallow were developed in Es4, paralleling to the trend of master fault with composite form.

Key words: associated deposits of terminal fan to beach-bar, sedimentary model, depositional evolution, sand distribution, Weicheng oilfield, Dongpu depression

中图分类号: 

  • P59
[1] 商晓飞, 侯加根, 程远忠, 等. 厚层湖泊滩坝砂体成因机制探讨及地质意义:以黄骅坳陷板桥凹陷沙河街组二段为例[J]. 地质学报, 2014, 88(9):1705-1718. Shang Xiaofei, Hou Jiagen, Cheng Yuanzhong, et al. Formation Mechanism of the Thick Layer Lacustrine Beach-Bar and Its Geological Implications:An Example of the 2nd Member of the Shahejie Formation in Banqiao Sag[J]. Acta Geologica Sinica, 2014, 88(9):1705-1718.
[2] 商晓飞, 侯加根, 董越, 等. 板桥凹陷同沉积断层主控的滩坝砂体沉积机制与分布样式[J]. 中国石油大学学报(自然科学版), 2014, 38(6):32-39. Shang Xiaofei, Hou Jiagen, Dong Yue, et al. Sedimentary Mechanism and Distribution Pattern of Beach-Bar Sandbodies Mainly Dominated by Contemporaneous Faults in Banqiao Sag[J]. Journal of China University of Petroleum (Edition of Natural Science), 2014, 38(6):32-39.
[3] 王山章, 张金亮, 徐淑娟. 卫城油田卫22块储层非均质性评价[J]. 中国海洋大学学报(自然科学版), 2011, 41(3):75-80. Wang Shanzhang, Zhang Jinliang, Xu Shujuan. Reservoir Heterogeneity Evaluation of Wei 22 Block in Weicheng Oilfield[J]. Periodical of Ocean University of China, 2011, 41(3):75-80.
[4] 刘永春, 李晓平, 王波, 等. 卫81块沙四段储层沉积微相及剩余油分布研究[J]. 断块油气田, 2001, 8(5):42-46. Liu Yongchun, Li Xiaoping, Wang Bo, et al. The Sedimentary Microfacies of Reservoirs and the Features of Remaining Oil Distribution in the Fourth Member of Wei81 Fault-Block in Weicheng Oilfield[J]. Fault-Block Oil & Gas Field, 2001, 8(5):42-46.
[5] 刘克奇, 田海芹, 王正蕾, 等. 卫城81断块沙四段沉积微相与储层非均质性[J]. 西南石油学院学报, 2005, 27(1):1-4. Liu Keqi, Tian Haiqin, Wang Zhenglei, et al. The Sedimentary Microfacies and Reservoir Heterogeneity in the Fourth Member of Shahejie Formation of Fault Block 81 in Weicheng Oilfield[J]. Journal of Southwest Petroleum Institute, 2005, 27(1):1-4.
[6] 徐淑娟. 卫城油田卫22断块精细地质模型与剩余油分布研究[D]. 青岛:中国海洋大学, 2010. Xu Shujuan. Research on Geological Modeling and Remaining Oil Distribution of Block Wei 22 in Weicheng Oilfield[D]. Qingdao:Ocean University of China, 2010.
[7] 张翼. 卫城油田卫81块沙河街组四段高分辨率层序地层学与沉积相研究[D]. 青岛:中国海洋大学, 2013. Zhang Yi. High-Resolution Sequence Stratigraphy and Sedimentary Facies Research of the 4th Member of Shahejie Formation of Weicheng Oilfield[D]. Qingdao:Ocean University of China, 2013.
[8] 刘景东, 蒋有录. 东濮凹陷北部地区古近系烃源岩热演化特征及其主控因素[J]. 中国地质, 2013, 40(2):498-507. Liu Jingdong, Jiang Youlu. Thermal Evolution Characteristics of Paleogene Source Rocks and Their Main Controlling Factors in Northern Part of Dongpu Depression[J]. Geology in China, 2013, 40(2):498-507.
[9] 李维禄. 卫城油田卫81块三维地质建模与剩余油分布规律研究[D]. 青岛:中国海洋大学, 2013. Li Weilu. Research on 3D Geological Modeling and Remaining Oil Distribution of Block Wei81 in Weicheng Oilfield[D]. Qingdao:Ocean University of China, 2013.
[10] Cross T A. High-Resolution Stratigraphic Correlation from the Perspective of Base-level Cycles and Sediment Accommodation[M]//Dolson J. Unconformity Related Hydrocarbon Exploration and Accumulation in Clastic and Carbonate Settings, Short Course Notes. Denver:Rocky Mountain Association of Geologists, 1991:28-41.
[11] 赵澄林. 沉积学原理[M]. 北京:石油工业出版社, 2001:16-30. Zhao Chenglin. Principles of Sedimentology[M]. Beijing:Petroleum Industry Press, 2001:16-30.
[12] 李维禄, 徐怀民, 高思宇, 等. 三角洲改造背景的浪控滨岸砂体成因类型及展布特征:以塔里木盆地东河塘地区"东河砂岩"为例[J]. 中国海洋大学学报(自然科学版), 2017, 47(9):86-95. Li Weilu, Xu Huaimin, Gao Siyu, et al. Genetic Types and Distribution Features of Wave-Dominated Shore Deposits with Reworked-Delta Background:A Case of ‘Donghe Sandstones’ in Donghetang Oilfield, Tarim Basin[J]. Periodical of Ocean University of China, 2017, 47(9):86-95.
[13] Li Weilu, Xu Huamin, Niu Yujie, et al. Sand Body Types of Clastic Shore Deposits with Delta Backgrounds and Their Control Over Reservoir Quality[J]. Arabian Journal of Geoscience, 2016, 9(4):1-13.
[14] Hampson G J, Stroms J E A. Geomorphological and Sequence Stratigraphic Variability in Wave-Dominated, Shoreface-Shelf Parasequences[J]. Sedimentology, 2003, 50(4):667-701.
[15] 张金亮, 司学强. 断陷湖盆碳酸盐与陆源碎屑组合沉积:以东营凹陷金家地区古近系沙河街组第四段上亚段为例[J]. 地质论评, 2007, 53(4):448-453. Zhang Jinliang, Si Xueqiang. Mixed Siliciclastic-Carbonate Sediment in Rift Lacustrine Basin:A Case on the Upper Part of the Fourth Member of the Eogene Shahejie Formation in Jinjia Area, Dongying Depression[J]. Geology Review, 2007, 53(4):448-453.
[16] 林敉若, 操应长, 葸克莱, 等. 阜康凹陷东部斜坡带二叠系储层特征及控制因素[J]. 吉林大学学报(地球科学版), 2018, 48(4):991-1007. Lin Miruo, Cao Yingchang, Xi Kelai, et al. Characteristics and Controlling Factors of Permian Reservoirs in Eastern Slope of Fukang Sag[J]. Journal of Jilin University (Earth Science Edition), 2018, 48(4):991-1007.
[17] 刘海, 林承焰, 张宪国, 等. 孔店油田馆陶组辫状河储层构型及剩余油分布规律[J]. 吉林大学学报(地球科学版), 2018, 48(3):665-677. Liu Hai, Lin Chengyan, Zhang Xianguo, et al. Reservoir Architecture and Remaining Oil Distribution in Braided River of Guantao Formation, Kongdian Oilfield[J]. Journal of Jilin University (Earth Science Edition), 2018, 48(3):665-677.
[18] 李慧明, 于兴河, 李胜利. 东濮凹陷南部沙三段物源分析[J]. 石油天然气学报, 2012, 34(1):12-15. Li Huiming, Yu Xinghe, Li Shengli. Es3 Provenance Analysis in the South of Dongpu Depression[J]. Journal of Oil and Gas Technology, 2012, 34(1):12-15.
[19] Newell A J, Tverdokhlebov V P, Benton M J. Interplay of Tectonics and Climate on A Transverse Fluvial System, Upper Permian, Southern Uralian Foreland Basin, Russia[J]. Sedimentary Geology, 1999, 127:11-29.
[20] 张金亮, 戴朝强, 张晓华. 末端扇:在中国被忽略的一种沉积作用类型[J]. 地质论评, 2007, 53(2):170-179. Zhang Jinliang, Dai Zhaoqiang, Zhang Xiaohua. Terminal Fan:A Type of Sedimentation Ignored in China[J]. Geological Review, 2007, 53(2):170-179.
[21] 孙乐, 于兴河, 李胜利, 等. 北部湾盆地乌石凹陷东区古近系流沙港组二段砂泥薄互层沉积相特征及演化[J]. 古地理学报, 2017, 19(6):1023-1026. Sun Le, Yu Xinghe, Li Shengli, et al. Sedimentary Characteristics and Evolution of Thin Interbeds of the Member 2 of Paleogene Liushagang Formation in Eastern Wushi Sag, Beibu Wan Basin[J]. Journal of Palaeogeography, 2017, 19(6):1023-1026.
[22] 杨勇强, 邱隆伟, 姜在兴, 等. 陆相断陷湖盆滩坝沉积模式:以东营凹陷古近系沙四上亚段为例[J]. 石油学报, 2011, 32(3):417-423. Yang Yongqiang, Qiu Longwei, Jiang Zaixing, et al. A Depositional Pattern of Beach Bar in Continental Rift Lake Basins:A Case Study on the Upper Part of the Fourth Member of the Shahejie Formation in the Dongying Sag[J]. Acta Petrolei Sinica, 2011, 32(3):417-423.
[23] 姜在兴, 王俊辉, 张元福. 滩坝沉积研究进展综述[J]. 古地理学报, 2015, 17(4):427-440. Jiang Zaixing, Wang Junhui, Zhang Yuanfu. Advances in Beach-Bar Research:A Review[J]. Journal of Palaeogeography, 2015, 17(4):427-440.
[24] 张鑫, 张金亮. 惠民凹陷中央隆起带沙四上亚段滩坝与风暴岩组合沉积[J]. 沉积学报, 2009, 27(2):246-252. Zhang Xin, Zhang Jinliang. Composite Deposits of Beach Bar and Tempestite in the Upper Fourth Member of Shahejie Formation in the Central Uplift Belt of Huimin Depression[J]. Acta Sedimentologica Sinica, 2009, 27(2):246-252.
[25] 邓宏文, 高晓鹏, 赵宁, 等.济阳坳陷背部断陷湖盆陆源碎屑滩坝成因类型、分布规律与成藏类型[J]. 古地理学报, 2010, 12(6):737-747. Deng Hongwen, Gao Xiaopeng, Zhao Ning, et al. Genetic Types, Distribution Patterns and Hydrocarbon Accumulation in Terrigenous Beach and Bar in Northern Faulted-Lacustrine-Basin of Jiyang Depression[J]. Journal of Palaeogeography, 2010, 12(6):737-747.
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