S. Yurtmen et G. Rowbotham, A scanning electron microscope study of post-depositional changes in the northeast Nigde ignimbrites, South Central Anatolia, Turkey, MINERAL MAG, 63(1), 1999, pp. 131-141
The ignimbrites of the northeast Nigde area, which are subdivided into the
Lower, Middle and Upper ignimbrites on the basis of their compositional and
stratigraphical characteristics, display textural variations from the base
to the top. A large proportion of these ignimbrites have been altered and
recrystallized by the processes of compaction, welding and devitrification,
and as a result of volatile movement. The alteration and recrystallization
processes include four stages: hydration, glassy and spherulitic stages ac
companied by vapour-phase crystallisation. In the early phases of devitrifi
cation, detailed shard shapes are easily recognisable with the scanning ele
ctron microscope. but as alteration proceeds clarity of detail disappears b
ecause compaction results in collapse of the structure of the rock. Spherul
itic and vapour-phase crystallisation usually involves the growth of alkali
feldspar and cristobalite. These later stages are more common in the Upper
Ignimbrite than the Middle and Lower ignimbrites.