Journal of Jilin University(Earth Science Edition) ›› 2016, Vol. 46 ›› Issue (1): 11-22.doi: 10.13278/j.cnki.jjuese.201601102

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Types and Characteristics of Volcanic Reservoir Pore-Fracture Units of Cretaceous Yingcheng Formation in Songliao Basin, NE China

Xiu Lijun1,2, Shao Mingli2, Tang Huafeng3, Dong Changchun2, Gao Youfeng3   

  1. 1. Institute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, China;
    2. Research Institute of Exploration and Development, Jilin Oilfield Company, Songyuan 138000, Jilin, China;
    3. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2015-04-09 Online:2016-01-26 Published:2016-01-26
  • Supported by:

    Supported by National Natural Science Foundation-Youth Foundation(41002038)and National Key Basic Research Program of China (2012CB822002)

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Abstract:

To evaluate volcanic reservoirs, only the parameters of porosity and permeability are now focused; while the void space, which is the controlling factor to influence the porosity and permeability, is ignored. It hampers the research of volcanic reservoirs. Types of pore-fracture units and their porosity and permeability are analyzed based on the cores of Yingcheng Formation in Early Cretaceous of well Y1D1 and well Y3D1 in Songliao basin. The main results are followings:1)There are five kinds of primary pores,three kinds of secondary pores,three kinds of primary fractures, and three kinds of secondary fractures. The most pores and fractures have been reformed by compaction and dissolution. According to the formation process and distribution pattern, the reservoir spaces are assembled to seven kinds of pore-groups and two kinds of fracture-groups. On the basis of combined characteristics of pore groups and fracture groups, the volcanic reservoirs are divided into seven types of pore-fracture units as below:unit ① assembling of scatter vesicles group (SVG) and secondary fracture group (SFG), unit ② assembling of directional vesicles group (DV), devitrification pore group (DPG) and SFG, unit ③ assembling of scatter intergranular pores group (SIPG) and emposieu group(EG), unit ④ assembling of SIPG, EG, and primary fracture group(PFG), unit ⑤ assembling of SIPG, EG, and SFG, unit ⑥ assembling of directional intergranular pores group (DIPG), EG, and SFG, and unit ⑦ assembling of PFG and SFG. 2)The porosity and permeability of the pore-fracture units have high value except unit ② and unit ⑦. There are three groups of slope of correlation function of pore-fracture units between porosity and permeability comparing to that of the total samples. Group A includes unit ① and ②, whose slope is smaller than the total's; Group B includes unit ③,④,⑤ and ⑥, whose slope is bigger than the total's; Group C is unit ⑦, whose slope is much bigger than the total's. 3) The pore throat sorting coefficient of pore-fracture units are positive correlation with pore throat average radius; this means that the heterogeneity of reservoir becomes stronger. Most pore-fracture units consist of complex lithology and lithofacies. The distribution characteristics of pore-fracture units are correlated to the types and facies belts of volcanic edifices. Based on the above, for reservoir evaluation, the pore-fracture units have also to be considered in addition to their parameters of porosity, permeability, and correlation function; although the units ① and unit ② bear in lava, they have distinct characteristics in porosity and permeability, and it is necessary to treat them individually.

Key words: Songliao basin, Yingcheng Formation, volcanic rocks, pore-fracture units, void space

CLC Number: 

  • P618.18

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