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岩石中纳米粒子层的观察厘定及其地质意义

孙岩 陆现彩 舒良树 刘浩

孙岩, 陆现彩, 舒良树, 等, 2008. 岩石中纳米粒子层的观察厘定及其地质意义. 地质力学学报, 14 (1): 37-44.
引用本文: 孙岩, 陆现彩, 舒良树, 等, 2008. 岩石中纳米粒子层的观察厘定及其地质意义. 地质力学学报, 14 (1): 37-44.
SUN Yan, LU Xian-cai, SHU Liang-shu, et al., 2008. OBSERVATION AND DETERMINATION OF THE NANO-SIZED PARTICLE LAYER IN ROCKS AND ITS GEOLOGICAL SIGNIFICANCE. Journal of Geomechanics, 14 (1): 37-44.
Citation: SUN Yan, LU Xian-cai, SHU Liang-shu, et al., 2008. OBSERVATION AND DETERMINATION OF THE NANO-SIZED PARTICLE LAYER IN ROCKS AND ITS GEOLOGICAL SIGNIFICANCE. Journal of Geomechanics, 14 (1): 37-44.

岩石中纳米粒子层的观察厘定及其地质意义

基金项目: 

油气藏地质及开发工程国家重点实验室(西南石油学院)基金项目 PLN0606

国家自然科学基金 40634022

详细信息
    作者简介:

    孙岩(1937-), 男, 教授, 博士生导师, 1960年毕业于南京大学地质学系, 长期从事构造地质学、石油地质学和显微构造学方面的教学科研工作

  • 中图分类号: P583

OBSERVATION AND DETERMINATION OF THE NANO-SIZED PARTICLE LAYER IN ROCKS AND ITS GEOLOGICAL SIGNIFICANCE

  • 摘要: 纳米粒子具有个体极小(≤ 100nm), 大小均一, 多元物质和功能繁多的特点。岩石剪切滑移面纳米粒子层最早发现于美国圣安德列斯断裂带的花岗质糜棱岩中, 后相继在国内外一些地区的不同岩类中观察到。在剪切滑动作用下, 具有圆度和球度的纳米粒子可被变异, 并形成层状结构和各种构造型式。对岩石中纳米粒子层的成因有着不同的观点, 我们倾向于剪切摩擦的主导作用, 纳米粒子层可称谓摩擦-粘性薄层带。纳米级尺度粒子的力学、物理和化学效应是多种的、新奇的, 因此, 岩石纳米粒子层的研究有着重要的理论和实践意义。目前有关方面的研究工作, 国内外都处在起步阶段。

     

  • 1a  页岩的细碎屑结构

    1a.  Fine clastic texture in shale

    1b  密集展布的纳米粒子(ab面)和X型构造(箭头示)(Photo No.4567)

    1b.  Closely spaced nano-sized particles (ab plane)and X-type structure (shown by an arrow)

    图  2  个体纳米颗粒集结成复体颗粒(ab面)(Photo No.550)

    Figure  2.  Compound particles formed by clustering of single nano-sized ones (ab fabric plane)(Photo No.550)

    图  3  密集纳米颗粒成层状结构(ac面)(Photo No.2950)

    Figure  3.  Layered texture with close-spaced nano-sized particles (ab fabric plane)

    4a  纳米线组成的似帚状构造(ab面)(Photo 4583)

    4a.  Broom-like structure composed by nano-sized lines (ab fabric plane)

    4b  图 4a (左边)局部放大(ab面)(Photo 4585)

    4b.  Partial magnification (left side)of Fig. 4a (ab fabric plane)

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出版历程
  • 收稿日期:  2008-01-03
  • 刊出日期:  2008-03-28

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