| W油藏粘土矿物特征及油层低阻成因 |
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| 引用本文： | 廖明光,苏崇华,唐 洪,姜 巍.W油藏粘土矿物特征及油层低阻成因[J].西南石油大学学报（社会科学版）,2011,32(5):70-74. |
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| 作者姓名： | 廖明光 苏崇华 唐 洪 姜 巍 |
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| 作者单位： | 1.西南石油大学资源与环境学院，四川 成都 610500； 2.中海石油有限公司湛江分公司研究院，广东 湛江 524057；3.中国石油川庆钻探公司地质勘探开发研究院，四川 成都 610051 |
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| 摘 要： | W油藏Z1油组为高孔低渗低阻油藏，低阻油层的地质成因复杂多样。依据Z1油组储层发育特征，研究了储层粘土矿物的类型、颗粒的分布形式和泥质含量，以及上述粘土矿物特征对Z1油组低阻的影响。研究发现，Z1油组低阻层段的粘土类型以伊蒙混层为主，其相对含量高；粘土颗粒较均匀地成薄膜状、絮状分布；平均泥质含量高。粘土矿物组构产生的附加导电性和高泥质含量是影响Z1油组低电阻率的重要因素之一。
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| 关 键 词： | 低电阻率油层 粘土矿物 附加导电性 泥质含量 低阻成因 |
CHARACTERISTICS OF CLAY MINERALS IN W LOW RESISTIVITY RESERVOIRS AND THE GENESIS OF LOW RESISTIVITY |
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| LIAO Ming-guang,SU Chong-hua,TANG Hong,JIANG Wei.CHARACTERISTICS OF CLAY MINERALS IN W LOW RESISTIVITY RESERVOIRS AND THE GENESIS OF LOW RESISTIVITY[J].Journal of Southwest Petroleum University(Social Sciences Edition),2011,32(5):70-74. |
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| Authors: | LIAO Ming-guang SU Chong-hua TANG Hong JIANG Wei |
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| Institution: | 1.School of Resources and Environment,Southwest Petroleum University,Chengdu Sichuan 610500,China;2.Research Institute of Exploration and Development,Zhanjiang Company,CNOOC,Zhanjiang Guangdong 524057,China;3.Research Institute of Exploration and Development,Chuanqing Drilling & Exploration Company,CNPC,Chengdu Sichuan 610051,China |
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| Abstract: | The reservoir of Z1 oil group in W Oilfield has low resistance,high-porosity and low permeability.The geological formation of low resistivity reservoir has many reasons.In view of the developing features of Z oil group,the clay minerals types,clay particles distribution,clay content and the influence of them on the low-resistivity are studied.It can be found that the clay types in low resistivity layer segment of Z1 oil group is mainly the mixed layer of illite and montomorillonite and the content is relatively high.The clay particles are evenly distributed in a thin film and in flocculating form with high average clay content.Additional conductivity caused by clay minerals and high clay content are the main factors affecting the low resistivity of Z1 oil group. |
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| Keywords: | low-resistivity reservoir clay minerals additional conductivity clay content genesis of low resistivity |
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