Intensity Anomaly in Kikuchi Lines of Molybdenite.

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概要

• 論文の詳細を見る

• Kikuchi patterns of normal and anomalous molybdenites [Uyeda: Acta Cryst. A24 (1968) 175] were taken with a high voltage electron microscope at 350 kV and 500 kV. Many of the Kikuchi lines were indexed systematically. The normal molybdenite is polytype 2H_1, as is known, and the anomalous one is likely to be 2H_2 or 2T. The anomalous extinction of 400 and 700, as pointed out by Uyeda, was observed for the normal molybdenite, while their structure factors do not vanish. It is concluded that this effect is not due to another polytype, but to a dynamical many-beam interaction.

• 社団法人応用物理学会の論文
• 1968-11-05

著者

• Takahashi Hidewo

  Department Of Physics Nagoya University:(present Address) Department Of Geology Faculty Of Education

• Takahashi Hidewo

  Department Of Geology Faculty Of Education Kagoshima University

関連論文

• Group-Theoretical Method in the Many-Beam Theory of Electron Diffraction
• Intensity Anomaly in Kikuchi Lines of Molybdenite.

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