Lithologic Reservoirs ›› 2022, Vol. 34 ›› Issue (3): 82-92.doi: 10.12108/yxyqc.20220308

• PETROLEUM EXPLORATION • Previous Articles     Next Articles

Hydrocarbon accumulation conditions and main controlling factors of Paleogene in Chenghai slope,Huanghua Depression

GUO Meijie1, SHI Baohong1, DONG Xiongying2, LI Haodong2, HE Chuan2   

  1. 1. School of Earth Sciences and Engineering, Xi' an Shiyou University, Xi' an 710065, China;
    2. Research Institute of Exploration and Development, PetroChina Dagang Oilfield Company, Tianjin 300280, China
  • Received:2021-11-05 Revised:2022-01-11 Online:2022-05-01 Published:2022-05-12

Abstract: Based on the data of crude oil characteristics,thin section identification,scanning electron microscope and reservoir physical properties,the hydrocarbon accumulation law and main controlling factors of Paleogene in Chenghai slope of Huanghua Depression were studied. The results show that: (1)Two sets of main source rocks are developed in the first and third members of Paleogene in Chenghai slope,the organic matters are mainly typeⅡ1 and type Ⅱ2,with sufficient oil sources. The reservoir pores are mainly intergranular dissolved pores, intragranular dissolved pores and moldic pores. Three high-quality pore zones are developed vertically. Differential pressure hydrocarbon expulsion provides power for oil and gas migration,and different combinations of faults and reservoirs form a variety of fault lithologic traps.(2)The main controlling factors of hydrocarbon accumulation in the high part of the slope are sand bodies and unconformity surface as oil and gas migration channel, and the main controlling factor of hydrocarbon accumulation in the middle part of the slope is fault. The low part of the slope is close to the oil source and has sufficient hydrocarbon supply,so the reservoir has become the key factor for its accumulation.(3)The low part of the slope is the main controlling factor for hydrocarbon enrichment. The reservoir conditions in the high part of the slope are the best,but the hydrocarbon supply is insufficient. There are many faults in the middle part of the slope,and the fault activity can provide good migration and preservation conditions for hydrocarbon accumulation. The low part of the slope has sufficient hydrocarbon supply, but the reservoir conditions are poor,so the middle part of the slope is the block with the most abundant oil and gas resources.

Key words: accumulation conditions, enrichment law, slope part, Paleogene, Chenghai slope, Huanghua Depression

CLC Number: 

  • TE122
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[1] WEI Qinlian, ZHENG Rongcai, XIAO Ling,WANG Chengyu, NIU Xiaobing. Influencing factors and characteristics of Chang 6 reservoir in Wuqi area, Ordos Basin[J]. Lithologic Reservoirs, 2007, 19(4): 45 -50 .
[2] WANG Dongqi, YIN Daiyin. Empirical formulas of relative permeability curve of water drive reservoirs[J]. Lithologic Reservoirs, 2017, 29(3): 159 -164 .
[3] LI Yun, SHI Zhiqiang. Study on fluid inclusion of tight sandstone reservoir of Upper Triassic Xujiahe Formation in central Sichuan Basin[J]. Lithologic Reservoirs, 2008, 20(1): 27 -32 .
[4] JIANG Ren, FAN Tailiang, XU Shouli. Concept and techniques of seismic geomorphology[J]. Lithologic Reservoirs, 2008, 20(1): 33 -38 .
[5] ZOU Mingliang, HUANG Sijing, HU Zuowei, FENG Wenli, LIU Haoniannian. The origin of carbonate cements and the influence on reservoir quality of Pinghu Formation in Xihu Sag, East China Sea[J]. Lithologic Reservoirs, 2008, 20(1): 47 -52 .
[6] WANG Bingjie, HE Sheng, NI June, FANG Du. Activity analysis of main faults in Qianquan area, Banqiao Sag[J]. Lithologic Reservoirs, 2008, 20(1): 75 -82 .
[7] CHEN Zhenbiao, ZHANG Chaomo, ZHANG Zhansong, LING Husong, SUN Baodian. Using NMR T2 spectrum distribution to study fractal nature of pore structure[J]. Lithologic Reservoirs, 2008, 20(1): 105 -110 .
[8] ZHANG Houfu, XU Zhaohui. Discussion on stratigraphic-lithologic reservoirs exploration in the aspect of the research history of reservoirs[J]. Lithologic Reservoirs, 2008, 20(1): 114 -123 .
[9] ZHANG Xia. Cultivation of exploration creativity[J]. Lithologic Reservoirs, 2007, 19(1): 16 -20 .
[10] YANG Wuyang, YANG Wencai, LIU Quanxin, WANG Xiwen. 3D frequency and space domain amplitude-preserved migration with viscoelastic wave equations[J]. Lithologic Reservoirs, 2007, 19(1): 86 -91 .
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