Lithologic Reservoirs ›› 2014, Vol. 26 ›› Issue (6): 57-63.doi: 10.3969/j.issn.1673-8926.2014.06.010

Previous Articles     Next Articles

Study on sedimentary facies of the third member of Shahejie Formation in Lin 7 fault block, Huimin Sag

LUO Wei1, HE Youbin2, MA Bo3
  

  1.  1. Research Institute of Petroleum Prospecting and Development , Sinopec East China Subsidiary Company , Nanjing 210011 , China ; 2. School of Geoscience , Yangtze University , Wuhan 430100 , China ; 3. Headquarters of Unconventional Oil and Gas Resources Prospecting and Development ,
    Sinopec East China Subsidiary Company , Nanjing 210011 , China
  • Online:2014-11-20 Published:2014-11-20

Abstract:

Based on core observation, combining with data of regional geology, analysis assay and well logging, this paper systematically studied the sedimentary facies of the third member of Shahejie Formation ( Es 3 ) in Lin 7 fault block of Huimin Sag. It is considered that the study area developed delta, turbidite fan and lacustrine facies. The delta can be further divided into microfacies of underwater distributary channel, interdistributay bay, mouth bar, distal bar and prodelta mud, the turbidite fan can be further divided into microfacies of channel, interchannel, lateral frontchannel, margin channel and outer fan mud, and the lacustrine facies mainly developed semi-deep to deep lake mud. In the plan, the sediment in Es 3 spreaded along WN-ES direction. In vertical profile, the delta deposite mainly developed in lower Es 3 , the turbidite fan and the semi-deep to deep lacustrine mainly developed in middle and upper Es 3 . From lower Es3 to upper Es 3 , sand body experienced progradation to retrogradation repeatedly, and moved from west to east gradually, and the water is deepening gradually on the whole, including some short decreasing. This study of sedimentary microfacies provides geological basis for the comprehensive reservoir research of Es 3 in Lin 7 fault block.

Key words:  flowunit , modified stratigraphic Lorenz plot , flowzone indicator , integrated index of reservoir hetero-geneity , pore throat aperture

[1]赵澄林,张善文,袁静,等.胜利油区沉积储层与油气[M].北京:石油工业出版社,1999:18-26.
[2]张福明.惠民凹陷中央隆起带沙三段储层预测研究[D].东营:中国石油大学(华东),2007.
[3]马川斌.临盘油田油藏分类地质评价研究[D].北京:中国石油大学(北京),2007.
[4]张勇,柳永清.惠民凹陷西部老第三系沙河街组三段三角洲体系及砂岩体沉积特征和演化规律[J].地质论评,2001,47(3):322-328.
[5]姜在兴,操应长,邱隆伟,等.砂体层序地层及沉积学研究:以山东惠民凹陷为例[M].北京:地质出版社,2000:15-68.
[6]孙以德,宋全友,刘苏,等.盘一东断块构造特征研究[J].内江科技,2006,(1):154 .
[7]何幼斌,王文广.沉积岩与沉积相[M].北京:石油工业出社,2006:33-42.
[8]《沉积构造与环境解释》编著组.沉积构造与环境解释[M].北京:科学出版社,1984:3-39.
[9]潘树新,郑荣才,卫平生,等.陆相湖盆块体搬运体的沉积特征、识别标志与形成机制[J].岩性油气藏,2013,25(2):9-18.
[10]刘宝珺,曾允孚.岩相古地理基础和工作方法[M].北京:地质出版社,1985:31-38.
[11]操应长,刘晖.湖盆三角洲沉积坡度带特征及其与滑塌浊积岩分布关系的初步探讨[J].地质论评,2007,53(4):454-459.
[12]郑荣才,郑哲,高博禹,等.珠江口盆地白云凹陷珠江组海底扇深水重力流沉积特征[J].岩性油气藏,2013,25(2):1-8.
[13]张鹏飞.东营凹陷洼陷带沙三中亚段浊积岩成藏条件分析[J].岩性油气藏,2012,24(3):61-65.
[14]夏景生,王志坤,陈刚,等.东营凹陷东部深层浊积扇油藏成藏条件与模式研究[J].岩性油气藏,2009,21(1):55-60.
[15]Mattern F. Ancient sand-rich submarine fans:Depositional systems, models,identification,and analysis[J]. Earth-Science Reviews,
[16]宋子齐,潘艇,程英,等.利用测井曲线研究沉积微相及其含油有利区展布[J].中国石油勘探,2007,(4):37-41.
[17]杨俊生,樊太亮.惠民凹陷古近系沙河街组三段沉积体系[J].新疆石油地质,2007,28(4):457-461.
[18]操应长,姜在兴,李春华,等.山东惠民凹陷中央隆起带古近系沙三段层序地层及沉积演化[J].古地理学报,2002,4(3):40-46.
[19]潘元林,张善文,肖焕钦,等.济阳断陷盆地隐蔽油气藏勘探[M].北京:石油工业出版社,2003:1-58.
[20]Akdag K,Kirmaci M Z. Submarine fan and slope-apron deposition.2005,70:167-202.
 
[1] LU Mingzhen,LIN Chengyan,ZHANG Xianguo,ZHANG Jiangtao . Evaluation and optimization of flow unit division methods [J]. LITHOLOGIC RESERVOIRS, 2015, 27(1): 74-80.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] . [J]. Lithologic Reservoirs, 2022, 34(2): 0 .
[2] LI Zaiguang,LI Lin. Automatic mapping based on well data[J]. Lithologic Reservoirs, 2007, 19(2): 84 -89 .
[3] CHENG Yuhong,GUO Yanru,ZHENG Ximing,FANG Naizhen,MA Yuhu. The interpretation method and application effect determined by multiple seismic and logging factors[J]. Lithologic Reservoirs, 2007, 19(2): 97 -101 .
[4] LIU Juntian,JIN Zhenjia,LI Zaiguang,TAN Xinping,GUO Lin,WANG Bo,LIU Yuxiang. Controlling factors for lithologic hydrocarbon reservoirs and petroleum prospecting target in Xiaocaohu area , Taibei Sag[J]. Lithologic Reservoirs, 2007, 19(3): 44 -47 .
[5] SHANG Changliang, FU Shouxian. Application of 3D seismic survey in loess tableland[J]. Lithologic Reservoirs, 2007, 19(3): 106 -110 .
[6] WANG Changyong, ZHENG Rongcai, WANG Jianguo, CAO Shaofang, Xiao Mingguo. Sedimentary characteristics and evolution of Badaowan Formation of Lower Jurassic in northwest margin of Junggar Basin[J]. Lithologic Reservoirs, 2008, 20(2): 37 -42 .
[7] WANG Ke1 LIU Xianyang, ZHAO Weiwei, SONG Jianghai, SHI Zhenfeng, XIANG Hui. Char acter istics and geological significance of seismites of Paleogene in Yangxin Subsag of J iyang Depr ession[J]. Lithologic Reservoirs, 2008, 20(2): 54 -59 .
[8] SUN Hongbin, ZHANG Fenglian. Structural-sedimentary evolution char acter istics of Paleogene in Liaohe Depr ession[J]. Lithologic Reservoirs, 2008, 20(2): 60 -65 .
[9] LI Chuanliang. Can uplift r esult in abnormal high pr essur e in formation?[J]. Lithologic Reservoirs, 2008, 20(2): 124 -126 .
[10] WEI Qinlian,ZHENG Rongcai,XIAO Ling,MA Guofu,DOU Shijie,TIAN Baozhong. Study on horizontal heterogeneity in Serie Inferiere of Triassic in 438b block , Algeria[J]. Lithologic Reservoirs, 2009, 21(2): 24 -28 .
TRENDMD: