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Abstract
Journal of Sedimentary Research, Section
A: Sedimentary Petrology and Processes
Vol. 65A (1995)No.
2. (April), Pages 332-336
A Model of Orientation of Subcrystals in Saddle Dolomite
Aleksandra Kostecka
ABSTRACT
Saddle dolomite crystals are composed of subcrystals that are slightly
overlapped, rotated, and tilted with respect to each other. The subcrystal
arrangement resembles a screw-like pattern. The c axes of subcrystals are
skew lines: their directions change from horizontal to steeply inclined
relative to the substrate. In thin section the traces of the c axes of
subcrystals simulate a divergent (or convergent) pattern, which is the
cause of sweeping extinction typical of saddle dolomite.
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