石油与天然气地质 ›› 2009, Vol. 30 ›› Issue (1): 47-52,58.doi: 10.11743/ogg20090107

• 石油地质理论 • 上一篇    下一篇

火山岩中脱玻化孔及其对储层的贡献

赵海玲1,2,3, 黄微3,4, 王成3,4, 狄永军1,2,3, 齐井顺3,4, 肖勇3, 刘杰4   

  1. 1. 中国地质大学, 地质过程与矿产资源国家重点实验室, 北京, 100083;
    2. 中国地质大学, 岩石圈构造、深部过程及探测技术教育部重点实验室, 北京, 100083;
    3. 中国地质大学, 北京, 100083;
    4. 中国石油天然气股份有限公司, 大庆油田有限责任公司石油勘探开发研究院, 黑龙江, 大庆, 163712
  • 收稿日期:2008-10-18 出版日期:2009-02-25 发布日期:2012-01-16
  • 基金资助:

    国家自然科学基金项目(40672088)

Micropores from devitrification in volcanic rocks and their contribution to reservoirs

Zhao Hailing1,2,3, Huang Wei3,4, Wang Cheng3,4, Di Yongjun1,2,3, Qi Jingshun3,4, Xiao Yong3, Liu Jie4   

  1. 1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China;
    2. Key Laboratory of Lithosphere Tectonics and Litho-probing Technology, Ministry of Education, China University of Geosciences, Beijing 100083, China;
    3. School of Geosciences and Resources, China University of Geosciences, Beijing 100083, China;
    4. Exploration and Development Research Institute, Daqing Oilfield Limited Company, Daqing, Heilongjiang 163712, China
  • Received:2008-10-18 Online:2009-02-25 Published:2012-01-16

PDF (PC)

683

被引次数

48

摘要：

岩相学研究表明火山岩中玻璃的脱玻化作用可以产生相当数量的微孔隙,所观察到的微孔隙为脱玻化孔和脱玻化形成的矿物与流体之间相互作用产生的孔隙之和,统称为脱玻化孔。球粒流纹岩、熔结凝灰岩中脱玻化孔是仅次于气孔的第二大孔隙类型,球粒流纹岩和熔结凝灰岩中脱玻化孔分别占相应岩石中所有类型孔隙的20%,30%左右。脱玻化孔是凝灰岩的主要孔隙类型,占凝灰岩中所有类型孔隙的70%左右。运用火山玻璃脱玻化作用的物理过程及质量平衡的原理和方法,可估算球粒流纹岩、熔结凝灰岩、凝灰岩中流纹质玻璃脱玻化作用产生的孔隙。运用流体-岩石相互作用的热力学原理和方法计算出长石溶蚀至少可以产生20 cm3/mol的孔隙。

关键词: 球粒流纹岩, 熔结凝灰岩, 凝灰岩, 脱玻化, 微孔隙, 火山岩

Abstract:

Petrography studies show that devitrification in volcanic rocks can produce a considerable number of micropores.The micropores observed in volcanic rocks are a complex of micropores from devitrification and that from interaction of minerals with fluids.In pyromerides and ignimbrites,micropores from devitrification are the second largest pore type after the vesicle,accounting for 20%and 30%of the total of all pore types in pyromerides and ignimbrites respectively.While in tuff,they are the predominant pore type and account for about 70%of the total pore spaces.The principles and methods of mass balance and the physical processes of devitrification can be used to estimate the micropores generated by devitrification of glass in pyromeride,ignimbrite and tuff.Calculation with the thermodynamical theories and methods of fluid-rock interaction shows that feldspar dissolution at least can produce pores of 20 cm3/mol.

Key words: pyromeride, ignimbrite, tuff, devitrification, micropore, volcanics

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