Yao Jingli, Chen Shijia, Lu Jungang, Zhang Huanxu, Liu Chaowei, Tang Haiping, Wang Gang, Zhang Bowei. Features and influencing factors of Chang 7 reservoir of Yanchang Formation in Hujianshan area, Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(2): 162-166. doi: 10.11781/sysydz201302162
Citation: Yao Jingli, Chen Shijia, Lu Jungang, Zhang Huanxu, Liu Chaowei, Tang Haiping, Wang Gang, Zhang Bowei. Features and influencing factors of Chang 7 reservoir of Yanchang Formation in Hujianshan area, Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(2): 162-166. doi: 10.11781/sysydz201302162

Features and influencing factors of Chang 7 reservoir of Yanchang Formation in Hujianshan area, Ordos Basin

doi: 10.11781/sysydz201302162
  • Received Date: 2012-07-26
  • Rev Recd Date: 2013-01-07
  • Publish Date: 2013-03-28
  • The Chang 7 strata in the Ordos Basin were regarded as source rocks in the past. Plenty of industrial oil wells have been found in the Chang 7 strata of the Yanchang Formation in Hujianshan area of the Ordos Basin in recent years; however, the reservoirs are unevenly distributed and have different industrial productivities. Based on rock thin section, cast thin section, mercury penetration and physical property analyses, the features of the Chang 7 reservoir were studied, and the influencing factors were discussed. Arkose and lithic arkose sandstones are most common in the Chang7 strata. The main interstitial materials are ferroan calcite and hydromica. Residual intergranular pore and dissolved pore are the dominant reservoir spaces. The Chang 7 reservoir is a low porosity and ultra-low permeability reservoir with micro-throat and poor physical property. The main affecting factors include quartz content, size of detrital grain, depositional micro-facies and diagenesis, etc.

     

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  • [1]
    张云峰,冯亚琴,徐涵,等.贝尔凹陷贝中次凹南屯组一段储层特征研究[J].地质科学,2011,46(2):510-517.
    [2]
    孟万斌,李敏,刘家铎,等.柴北缘潜西地区上干柴沟组储层特征与控制因素分析[J].成都理工大学学报:自然科学版,2011,38(5):487-493.
    [3]
    秦秋寒,宋效文,何成山,等.临江地区扶余—杨Ⅰ油层储层特征及主控因素[J].大庆石油学院学报,2011,35(3):39-44.
    [4]
    陈志海.特低渗油藏储层微观孔喉分布特征与可动油评价:以十屋油田营城组油藏为例[J].石油实验地质,2011,33(6):657-670.
    [5]
    蒋凌志,牛嘉玉,张庆昌,等.渤海湾盆地深部有利储层发育的主控因素[J].地质论评,2009,55(1):73-78.
    [6]
    张云峰,王国强,付宝利,等.长岭断陷深层碎屑岩储层成岩作用及异常高孔带成因[J].吉林大学学报:地球科学版,2011,41(2):372-376.
    [7]
    孙致学,鲁洪江,冯文光,等.低渗透砂岩储集层油藏评价一体化研究方法及应用[J].石油勘探与开发,2006,33(6):743-748.
    [8]
    胡望水,张宇规,牛世忠,等.相控储层地质建模研究[J].特种油气藏,2010,17(5):37-39.
    [9]
    陈全红,李文厚,高永祥,等.鄂尔多斯盆地上三叠统延长组深湖沉积与油气聚集意义[J].中国科学:D辑:地球科学,2007,37(增刊Ⅰ):39-48.
    [10]
    张伟,刘建朝,高志亮,等.鄂尔多斯盆地吴堡地区长6段浊积特征及其石油地质意义[J].地球科学与环境学报,2012,34(2):64-71.
    [11]
    郭正权,齐亚林,楚美娟,等.鄂尔多斯盆地上三叠统延长组储层致密史恢复[J].石油实验地质,2012,34(6):594-603.
    [12]
    王志辉,黄伟.鄂尔多斯盆地南部直罗油田长8油层油气沸腾包裹体群研究[J].地球科学与环境学报,2011,33(2):146-151.
    [13]
    杨希濮,孙卫.鄂尔多斯盆地低渗透油藏孔隙结构特征及影响因素分析[J].特种油气藏,2011,18(6):44-47.
    [14]
    方少仙,候方浩.石油天然气地质储层沉积学[M].北京:中国石油大学出版社,2002:124-143.
    [15]
    李道品.低渗透油田开发概论[J].大庆石油地质与开发,1997,16(3):33-37.
    [16]
    杨懿,姜在兴,张小莉,等.大牛地气田盒3段致密储层控制因素及测井岩相研究[J].西北大学学报:自然科学版,2010,40(4):699-707.
    [17]
    刘昊伟,郑兴远,陈全红,等.华庆地区长6深水沉积低渗透砂岩储层特征[J].西南石油大学学报,2010,32(1):21-26.
    [18]
    唐海发,彭仕宓,赵彦超,等.致密砂岩储层物性的主控因素分析[J].西安石油大学学报,2007,22(1):59-63.
    [19]
    付文耀,刘春武,刘丽丽,等.鄂尔多斯盆地胡尖山油田延长组长61储层特征及控制因素分析[J].石油天然气学报(江汉石油学院学报),2011,33(7):45-49.
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