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Determination of layer stacking microstructures and intralayer transition of illite polytypes by high-resolution transmission electron microscopy (HRTEM)

机译:高分辨率透射电子显微镜(HRTEM)测定伊利石多型的层堆积微结构和层内转变

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摘要

A detailed investigation of microstructures of authigenic illite has been carried out using high-resolution TEM. Near-atomic images of 1M and 2M1 polytypes of illite with incidence [100] and [110] were observed. We unambiguously determine 1M illite in both individual particles and microtwinned domains. Newly formed 2M1 domains are surrounded by former packets of 1Md or 1M illite. Such intergrowth of different illite-polytypic domains on a scale of several layers suggests that they are metastable. The lateral-coherent 1M and 2M1 illite domains are aligned along the same orientation and crystallographically continuous normal to [001]*. This is a new phenomenon observed for polytypic intergrowth and transition. The intralayer-stepwise change of stagger direction in a series of successive layers and consequently the interlayer-stacking angle change resulting in polytypic transition are hypothesized as an "intralayer-stepwise transition" model. It explains the process of illite polytypic transition in the solid state.
机译:使用高分辨率TEM对自生伊利石 的微观结构进行了详细研究。观察到伊利石1M和2M 1 多型的近原子 图像,其发生率分别为[100] 和[110]。我们明确地确定了单个颗粒和微孪晶域中的1M伊利石 。新形成的 2M 1 域被以前的1M d 1M伊利石包所包围。不同伊利石多型域 在几层尺度上的这种共生表明它们是亚稳的。 横向相干的1M和2M 1 伊利石域沿 相同的方向排列,并且在晶体学上连续的法线 对准[001] *。这是在多型共生 和过渡中观察到的新现象。假设连续序列中交错方向 的层内逐步变化以及因此导致多型过渡的层间堆叠 角度变化假定为 as “层内逐步过渡”模型。它解释了固态伊利石多型转变的 过程。

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  • 来源
    《American Mineralogist》 |2007年第6期|926-932|共7页
  • 作者

    Tao Chen; Hejing Wang;

  • 作者单位

    Key Laboratory of Orogenic Belts and Crustal Evolution (Peking University), Ministry of Education of China, School of Earth and Space Sciences, Peking University, Beijing 100871, China;

    Key Laboratory of Orogenic Belts and Crustal Evolution (Peking University), Ministry of Education of China, School of Earth and Space Sciences, Peking University, Beijing 100871, China;

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