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