J4 ›› 2011, Vol. 41 ›› Issue (4): 999-1005.

Previous Articles     Next Articles

Types and Study Significance of Abandoned Channel for PⅠ31 Layer in Xingnan Development Area

ZHAI Zhi-wei1|SHI Shang-ming1|ZHU Huan-lai1|SHI Jiang-bo2   

  1. 1.College of Earth Sciences, Northeast Petroleum University, Daqing163318, Heilongjiang, China;
    2.Exploration &|Development Institute, Daqing Oil Field Company Ltd., Daqing163712|Heilongjiang, China
  • Received:2010-10-09 Online:2011-07-26 Published:2011-07-26

Abstract:

When the oil fields exploration enters the period of high water-cut, fine description of reservoir structure is of great significance to improve the effect of oil exploration. As abandoned channels are important basis for identification of point-bar sand bodies and single channels boundary, the mud or sand and shale inter bedded sedimentary on the top of abandoned channels keeps off fluids in reservoir, so it is essential scientific basis for analyzing reservoir structure deeply and tapping remaining oil to identify the abandoned channels correctly. We take PⅠ31 layer in Xingnan development area for example, by analyzing the plane and section sedimentary characters of abandoned channels, utilizing method of relative depth contour of sand top, combining plane patterns of sand distribution and log curves response characteristics of abandoned channels, 26 abandoned channels of different size are identified in PⅠ31 layer of the area, and the width is generally around 100 m. Compared with gradually disposable abandoned channels, three sudden disposable abandoned channels sand bending degree is even bigger and extension range is shorter, and the sedimentary thickness is between 2 and 8 meters. As the lateral block action of inter bedded sandstone and mudstone or mud stone, the semi-communicated sand body combined with abandoned channels and general channels brings about unbalanced injection and production system for having injection no production or having production no injection. Top of channels sand becomes favorable zone for collection of residual oil, which is the focal points for further excavation.

Key words: reservoir structure, single channel, point bar, abandoned channel, sedimentation, Daqing

CLC Number: 

  • P618.13
[1] Gao Xiang, Liu Zhihong, Nie Zhiyang, Yao Yong, Jia Wo, Wang Chao, Song Jian. Determination of Timing and Its Geological Significance of Daqing Placanticline in Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2017, 47(1): 74-83.
[2] Lin Chengyan, Cao Zheng, Ren Lihua, Zhang Changsheng, Fan Ruifeng, Wang Ye, Xing Xinya, Ma Xiaolan. Oil Enrichment Regularity and Accumulation Modes of Putaohua Reservoir in Daqingzijing Syncline Area,Southern Songliao Basin [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(6): 1598-1610.
[3] Kang Jian, Wei Qinghai, Zhou Lin, Gao Yan, Zhang Yonggang, Gao Feng. Deep Structure Based on Seismic Array Observations in Daqing Area [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(3): 900-910.
[4] Chen Yongsheng, Li Jianfen, Wang Fu, Tian Lizhu, Shang Zhiwen, Shi Peixin, Jiang Xingyu, Wang Hong. Records of Holocene Sedimentation Environment and Relative Sea Level by the Boreholes Collected Along the Present Shoreline of the West Coast of Bohai Bay, China [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(2): 499-517.
[5] Ma Boyong, Wang Genhou, Li Shanglin, Xu Hongyan. Characteristics of Mixed Sedimentations and Diagenesis of Terrigenous Clastic Rock and Carbonate:The Middle Jurassic in the East Qiangtang Basin, Tibet, China [J]. Journal of Jilin University(Earth Science Edition), 2015, 45(5): 1310-1321.
[6] Xu Dong, Chu Fengyou, Li Jiabiao, Yang Haili, Chen Liang. Transport and Deposition of Sediment on the Shelf off Western Guangdong to Northeastern Hainan [J]. Journal of Jilin University(Earth Science Edition), 2014, 44(3): 905-917.
[7] Chai Sheli, Gao Lina, Qiu Dianming, Chai Yuan, Guo Jia, Xu Xuechun. 210Pb and 137Cs Dating of the Sediment Core and  Its Recent Accumulation Rates in Yueliang Lake in West Jilin Province [J]. Journal of Jilin University(Earth Science Edition), 2013, 43(1): 134-141.
[8] LIU Zhi-hong, MEI Mei, LIU Hang-Jun, WU Xiang-mei, WAN Chuan-biao, LIN Dong-cheng, GAO Jun-yi. Extensional Fault-Bend Folding and Its Constrains on the Sedimentation of Beier Sag in Hailar Basin [J]. J4, 2012, 42(5): 1330-1337.
[9] TIAN Ji-jun, JIANG Zai-xing. Comparison and Analysis of Beach Bars Sedimentary Characteristics of Upper Es4 in Huimin and Dongying Depression [J]. J4, 2012, 42(3): 612-0623.
[10] GAO Zhi-qian, FAN Tai-liang, YANG Wei-hong, WANG Xin. Structure Characteristics and Evolution of the Eopaleozoic Carbonate Platform in Tarim Basin [J]. J4, 2012, 42(3): 657-665.
[11] CUI Ying-chun, SHI Xue-fa, LIU Ji-hua, MA Li-jie. Records of Past 70 Ma Dust Activities in Ferromanganese Crusts from Pacific Ocean [J]. J4, 2012, 42(2): 393-399.
[12] TANG Ji, LI Na, LI Hai-yi, BIAN Jian-min, LI Zhao-yang, CUI Yu-jun. Flux and Source Appointment of Heavy Metals from Atmospheric Dry and Wet Deposition in Daqing City, China [J]. J4, 2012, 42(2): 507-513.
[13] ZHANG Li-qiang. Direction of Sedimentary Provenance of the Neogene Guantao Formation in the Raoyang Depression [J]. J4, 2012, 42(2): 321-326.
[14] XU Sheng-chuan, LIU Zhao-jun, DONG Qing-shui, CHEN Hui-jun, LIU Rong. Deposition and Sedimentary Evolution of Coal, Oil Shale and EvaporiteBearing Strata in Terrestrial Basins [J]. J4, 2012, 42(2): 296-303.
[15] BAI Yun-feng, FENG Zhi-qiang, CHENG Ri-hui, REN Yan-guang, TANG Hua-feng. Depositional Sequence and Filling Response of Fuyu Oil Layer in Daqing Placanticline [J]. J4, 2012, 42(2): 312-320.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!