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准噶尔盆地莫西庄地区侏罗系三工河组二段储层特征
引用本文:李志明,秦建中,廖宗廷,施伟军,罗月明,范明,朱樱,刘伟新,尹伟. 准噶尔盆地莫西庄地区侏罗系三工河组二段储层特征[J]. 吉林大学学报(地球科学版), 2006, 36(5): 799-804
作者姓名:李志明  秦建中  廖宗廷  施伟军  罗月明  范明  朱樱  刘伟新  尹伟
作者单位:1.中石化石油勘探开发研究院 无锡石油地质研究所,江苏 无锡 214151;2.同济大学 海洋与地球科学学院,上海 200092;3.中石化石油勘探开发研究院,北京 100083
基金项目:中石化西部新区勘探指挥部科技项目
摘    要:利用多种方法对准噶尔盆地莫西庄地区侏罗系三工河组二段储层特征进行了分析。结果表明,其成分成熟度较低、结构成熟度较高,孔隙度主要属特低孔-中孔,渗透率属超低渗-中渗。当孔隙度大于10%时,储层的含油性受渗透率控制。主要孔隙类型为原生粒间孔、溶蚀-改造粒间孔和粒内溶孔,孔隙类别以特大孔为主,而喉道类别以微细喉为主。成岩作用类型主要为机械压实作用、胶结作用、溶蚀和交代作用,成岩阶段处于晚成岩期A亚期,成岩演化过程中,机械压实作用、胶结作用导致储层孔隙度减小约24.5%,同时因溶蚀作用使孔隙度增大约4.5%。

关 键 词:三工河组  储层  岩石学特征  孔、渗特征  孔隙结构  成岩作用  莫西庄地区  
文章编号:1671-5888(2006)05-0799-06
收稿时间:2005-11-07
修稿时间:2005-11-07

Reservoirs Features of the Second Member of Jurassic Sangonghe Formation in Moxizhuang Area of Junggar Basin, NW China
LI Zhi-ming,QIN Jian-zhong,LIAO Zong-ting,SHI Wei-jun,LUO Yue-ming,FAN Ming,ZHU Ying,LIU Wei-xin,YIN Wei. Reservoirs Features of the Second Member of Jurassic Sangonghe Formation in Moxizhuang Area of Junggar Basin, NW China[J]. Journal of Jilin Unviersity:Earth Science Edition, 2006, 36(5): 799-804
Authors:LI Zhi-ming  QIN Jian-zhong  LIAO Zong-ting  SHI Wei-jun  LUO Yue-ming  FAN Ming  ZHU Ying  LIU Wei-xin  YIN Wei
Affiliation:1.Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214151,China;2.School of Ocean and Earth Science, Tongji University, Shanghai 200092,China;3.Research Institute of Petroleum Exploration and Development, SINOPEC, Beijing 100083,China
Abstract:The reservoir features of second member of Jurassic Sangonghe Formation in Moxizhuang area of Junggar Basin, have been studied by various means. The results show that reservoir rocks have relatively low composition maturity and high geometry maturity. Porosity of the reservoirs mainly belongs to very low to middle standard and permeability mainly belongs to extremely low to middle standard. The oil-bearing condition of reservoir is mainly controlled by permeability when porosity is high to 10%. Main pore types are primary intergranular pore, corrosion-modification intergranular pore and intragranular corrosion pore. Pore family is dominated by special large pore and throat family is dominated by micro-throat. Diagenesis types are compaction, cementation, alteration and replacement, and diagenesis stage is at A sub-period of late diagenesis period. Compaction and cementation cause reservoir porosity decreasing about 24.5% and corrosion causes reservoir porosity increasing about 4.5% during the diagenesis period.
Keywords:Sangonghe Formation  reservoir  characteristics of petrology  characteristics of porosity and permeability  pore geometry  diagenesis  Moxizhuang area
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