Texture
Volume 1 (1972), Issue 2, Pages 111-115
doi:10.1155/TSM.1.111
X-Ray Analysis of a Quartz Fabric From the Sambagawa Crystalline Schist, Japan
1Institute of Geology and Mineralogy, Faculty of Science, Hiroshima University, Hiroshima, 730, Japan
2Mineralogischex Institut der Technischen Hochschule Darmstadt, 61 Darmstadt, Germany
Received 29 February 1972; Accepted 8 June 1972
Copyright © 1972 Hindawi Publishing Corporation. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
Abstract
An X-ray fabric analysis of quartz grains from the Sambagawa crystalline schist, Japan, whose c-axis fabric
(optically measured) was regarded as corresponding to an ultimate steady-state pattern of preferred orientation
of c-axes developed by the approximately non-rotational two-dimensional strain under the Sambagawa metamorphicconditions,
has been made by a texture goniometer for reflection. It has been clarified that [0001] and [10