赵海玲, 王成, 刘振文, 孙文亮, 卿忠, 陈令, 朱峰. 2009: 火山岩储层斜长石选择性溶蚀的岩石学及热力学研究. 地质通报, 28(4): 412-419.
    引用本文: 赵海玲, 王成, 刘振文, 孙文亮, 卿忠, 陈令, 朱峰. 2009: 火山岩储层斜长石选择性溶蚀的岩石学及热力学研究. 地质通报, 28(4): 412-419.
    ZHAO Hai-ling, WANG Cheng, LIU Zhen-wen, SUN Wen-liang, QING Zhong, CHEN Ling, ZHU Feng. 2009: Characteristics of petrology and thermodynamics of selective dissolution of plagioclase in volcanic reservoir rocks. Geological Bulletin of China. Geological Bulletin of China, 28(4): 412-419.
    Citation: ZHAO Hai-ling, WANG Cheng, LIU Zhen-wen, SUN Wen-liang, QING Zhong, CHEN Ling, ZHU Feng. 2009: Characteristics of petrology and thermodynamics of selective dissolution of plagioclase in volcanic reservoir rocks. Geological Bulletin of China. Geological Bulletin of China, 28(4): 412-419.

    火山岩储层斜长石选择性溶蚀的岩石学及热力学研究

    Characteristics of petrology and thermodynamics of selective dissolution of plagioclase in volcanic reservoir rocks. Geological Bulletin of China

    • 摘要: 长石溶孔是火山岩中重要的孔隙类型之一,火山岩的主要孔隙类型中长石溶孔所占的比例在1.24%~60.61%之间,在储层中占有重要地位。从岩相学、岩石化学CIPW标准矿物成分、热力学等方面论证了斜长石的选择性溶蚀。岩相学特征表现出斜长石选择性溶蚀的特征,即钙长石溶蚀时钠长石没有溶蚀,同时出现斜长石选择性溶蚀时钠长石和钾长石生长的现象。斜长石选择性溶蚀得到了CIPW标准矿物成分的支持,在CIPW标准矿物成分中长石的端元组分主要为钠长石和钾长石,而钙长石绝大多数为0或接近0。热力学研究表明,在同样的温度、压力和地层水成分的条件下,在斜长石中优先溶解钙长石组分。当地层水中Na+和K+浓度达到饱和时发生钠长石和钾长石沉淀,出现斜长石选择性溶蚀的同时发生钠长石和钾长石生长的现象。

       

      Abstract: Characteristics of petrology and thermodynamics of selective dissolution of plagioclase in volcanic reservoir rocks. Geological Bulletin of China

       

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