| 牛居地区下第三系砂岩储层中自生高岭石成因分析 |
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| 引用本文： | 车启鹏,孙洪斌,张凤莲,刘敏,李应暹.牛居地区下第三系砂岩储层中自生高岭石成因分析[J].吉林大学学报(地球科学版),1995(3). |
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| 作者姓名： | 车启鹏 孙洪斌 张凤莲 刘敏 李应暹 |
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| 作者单位： | 大庆石油学院，辽河石油勘探局勘探开发研究院 |
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| 摘 要： | 在详细工作基础上，指出本区砂岩中自生高岭石主要有四种成因、即在孔隙溶液中沉淀、长石的蚀变、白云母的转化及蒙皂石的转化等，并对每种成因进行了分析，指出了主要成因机制。
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| 关 键 词： | 长石，沉淀，蚀变，溶解，转化 |
AUTHIGENIC KAOLINITE ORIGN ANALYSIS OF PALEOGENE SANDSTONE RESERVOIRS IN NIUJU ARER |
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| CheQipeng.AUTHIGENIC KAOLINITE ORIGN ANALYSIS OF PALEOGENE SANDSTONE RESERVOIRS IN NIUJU ARER[J].Journal of Jilin Unviersity:Earth Science Edition,1995(3). |
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| Authors: | CheQipeng |
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| Institution: | CheQipeng(Daqing Petroleum Institute. Anda 151400)Sun Hongbin;zhang Fenglian;Liu Min;Li Yingxian(Exploration &Development Research Instirute of Liaohe Petroleum Bureau.Liaoning Panjin 124010) |
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| Abstract: | Based on the detailed study,the authors of the paper concluded that theauthigenic kaolinite in the paleogene sandstone mainly had four kinds of origins,theyare:precipitation from interstitial solution,alteration of feldspar,transformation ofmuscovite and smectite etc. After analysing each kind of origns,we believed the mainorign was the precipitation. |
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| Keywords: | feldspar precipitation alteration dissolve transformation |
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