ISSN 1673-8217 CN 41-1388/TE
主管:中国石油化工集团有限公司 主办:中国石油化工股份有限公司河南油田分公司
李泽民, 谭先锋, 薛伟伟, 邱雨, 雍玉婷, 刘志波. 2015: 碎屑岩中硅质胶结物物质来源及沉淀机理. 石油地质与工程, 29(02): 19-24+145-146.
引用本文: 李泽民, 谭先锋, 薛伟伟, 邱雨, 雍玉婷, 刘志波. 2015: 碎屑岩中硅质胶结物物质来源及沉淀机理. 石油地质与工程, 29(02): 19-24+145-146.
Li Zemin, . 2015: Material source of siliceous cement in clastic rock and the precipitation mechanism. Petroleum Geology and Engineering, 29(02): 19-24+145-146.
Citation: Li Zemin, . 2015: Material source of siliceous cement in clastic rock and the precipitation mechanism. Petroleum Geology and Engineering, 29(02): 19-24+145-146.

碎屑岩中硅质胶结物物质来源及沉淀机理

Material source of siliceous cement in clastic rock and the precipitation mechanism

  • 摘要: 在成岩演化过程中,硅质胶结物的参与是至关重要的,而硅质胶结物的特征、硅质来源及沉淀机理等非常复杂,往往由多种因素共同控制,很难分析单一因素的影响。从长石的溶蚀、黏土矿物的成岩蚀变、压溶压实作用、流体及其他来源对硅质胶结物的物质来源进行了讨论,并探讨pH值、离子强度、温度压力及表面特征等因素对硅质胶结物溶解沉淀的影响。结果表明,硅质胶结物的物质来源受多因素控制,不同沉积成岩环境差异较大;硅质胶结物的溶解沉淀也受多种因素共同控制、pH值在碱性范围、离子浓度越高、温度越高、压力越大就越有利于硅质胶结物的溶解,反之更利于硅质胶结物的沉淀。

     

    Abstract: During the diagenetic evolution,the participation of siliceous cement is very important.While the characteristics of the siliceous cement,silica source and the precipitation mechanism are very complicated,which are often controlled by a variety of factors,and it is difficult to analyze the influence of single factor.In this article from the dissolution of feldspar,clay minerals content of diagenetic alteration,and compaction,pressolution,fluid and other sources,the material sources of the siliceous cement have been discussed.Besides the effects of pH value,ionic strength,temperature,pressure and surface characteristics on dissolution precipitation siliceous cements have been also discussed.The results show that the siliceous cement material sources could be controlled by multiple factors,and the differences in different sedimentary diagenetic environment are bigger.Siliceous cement dissolution precipitation is controlled by various factors,in alkaline pH value,the higher the concentration,the higher the temperature,the greater the pressure is more conducive to the dissolution of siliceous cements,vice in favor of the precipitation of the siliceous cements.

     

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