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准西北缘哈山地区复杂构造带火山岩储层发育特征及成因模式
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  • 英文篇名:Development characteristics and genetic model of volcanic reservoir in complex tectonic belt of Hashan area,northwestern margin of Junggar Basin
  • 作者:于洪洲
  • 英文作者:YU Hongzhou;Exploration and Development Research Institute,Shengli Oilfield Company,SINOPEC;
  • 关键词:火山岩 ; 储集特征 ; 成因类型 ; 哈山地区 ; 准噶尔盆地
  • 英文关键词:volcanic rocks;;reservoir characteristics;;genetic types;;Hashan area;;Junggar Basin
  • 中文刊名:YQCS
  • 英文刊名:Petroleum Geology and Recovery Efficiency
  • 机构:中国石化胜利油田分公司勘探开发研究院;
  • 出版日期:2019-05-06 18:50
  • 出版单位:油气地质与采收率
  • 年:2019
  • 期:v.26;No.138
  • 基金:国家科技重大专项“准噶尔盆地碎屑岩层系油气富集规律与勘探评价”(2016ZX05002-002)
  • 语种:中文;
  • 页:YQCS201903006
  • 页数:8
  • CN:03
  • ISSN:37-1359/TE
  • 分类号:50-57
摘要
准噶尔盆地西北缘哈山地区属于山前复杂构造带,形成于陆缘岛弧环境的石炭系火山岩推覆体是该区重要的油气储集体。为分析复杂构造带火山岩储层发育特征及控制因素,利用大量露头、岩心、薄片、扫描电镜及成像测井等资料,对火山岩储集特征、影响因素及成储模式进行研究。结果表明:哈山地区石炭系火山岩主要由火山熔岩类的玄武岩、安山岩、玄武安山岩和火山碎屑岩类的火山角砾岩、凝灰岩2大类5种岩性组成;岩性和岩相是影响火山岩储层发育的内在因素,风化淋滤和构造作用是外在因素;储层成因包括岩相-断裂型和岩相-褶皱型2种类型;在推覆体的前翼和核部、断裂交汇处的风化壳、喷发旋回与期次界面处的火山角砾岩、凝灰岩、安山岩发育区是火山岩有利储层分布区。
        The Hashan area in the northwestern margin of Junggar Basin is a complex piedmont tectonic belt,in which the Carboniferous volcanic nappe forming in the continental margin island arc is an important oil and gas reservoir in this area.To understand the volcanic reservoir development characteristics and control factors in the complex tectonic belt,using a large number of outcrops,core,thin section,scanning electron microscopy and imaging logging analysis data,the characteristics of volcanic reservoir,influencing factors and accumulating model were studied.The results show that the carboniferous volcanic rock is mainly composed of 2 types and 5 kinds of lithology,including lava(basalt,andesite,and basaltic-andesite)and volcaniclastic rocks(volcanic breccia and tuff).Lithology and lithofacies are the internal factors influencing volcanic reservoirs development,while weathering and leaching and tectonism are the external factors.The genetic types of reservoirs include the lithofacies-fault type and the lithofacies-fold type.The volcanic breccia,tuff and andesite developing at the front wing and core of nappe,and weathering crust of faults intersection,and eruption cycle boundary are favorable distribution areas of volcanic reservoirs.
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