The effect of crystallographic orientation on pressure solution in quartzite

Автор(ы):Bas Den Brok
Издание:Journal of Structural Geology, 1996 г., 2 стр.
Язык(и)Английский
The effect of crystallographic orientation on pressure solution in quartzite

By measuring the degree of flattening and the orientation of the c-axis of single quartz grains in a naturally deformed ("cleaved") sandstone, Becker (1995) showed that: "quartz grains with a small angle between c-axis and the Z-axis of shortening exhibit the least amount of pressure solution, whereas grains with c-axes oriented at about 50° to Z manifest the highest degree of pressure solution". I briefly present some experimental results that show exactly the same. <...>

ТематикаКристаллография
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