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Tubular Form of Interstratified Mineral Consisting of a Serpentine-like Layer Plus Two Brucite-like Sheets Newly Found in the Murchison (C2) Meteorite

机译:管状形状的层状矿物由蛇纹状层加上两块类似于水蛭的板料在murchison(C2)陨石中新发现

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摘要

Phyllosilicates in the matrix of the Murchison meteorite can be morphologically classified into three types based on the observation by high resolution electron microscopy; phyllosilicate with extremely low crystallinity, platy phyllosilicate, and tubular phyllosilicate. A new type of phyllosilicate having both platy and tubular forms was found. It consists of an alternation of serpentine-like 1 : 1 layer and a couple of brucite-like sheets, and has 17 Å periodicity. One-dimensional electron microscopic images of this new type phyllosilicate are calculated and compared with the electron micrographs actually taken. The genesis of phyllosilicates and the process of formation of the tubular phyllosilicate in the Murchison meteorite are discussed.
机译:基于高分辨率电子显微镜的观察,Murchison陨石基质中的硅基硅酸盐可在形态上分为三类:结晶度极低的层状硅酸盐,板状层状硅酸盐和管状的层状硅酸盐。发现了一种具有板状和管状形式的新型页硅酸盐。它由蜿蜒的1:1层和几块水镁石片交替组成,具有17 17的周期性。计算这种新型页硅酸盐的一维电子显微图像,并将其与实际拍摄的电子显微照片进行比较。讨论了Murchison陨石中页硅酸盐的成因和管状页硅酸盐的形成过程。

著录项

  • 作者

    Junjii Akai;

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  • 年度 1980
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  • 原文格式 PDF
  • 正文语种 en
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