Acause for formation of rapakivi texture in porphiroid quartz monzonite massive of Akapol area
| Category | Petrology |
|---|---|
| Group | GSI.IR |
| Location | 23th symposium on geosciences |
| Holding Date | 05 May 2008 |
Abstract:
Rapakivi texture is seen mainly in quartz monzonite of Akapol area which is investigated based on petrography studies. In all investigated rapakivi textures, alkali feldspar owned rounded margins; which is surrounded by Plagioclase .
Existing of microgranoular enclaves mafic, poikilitic texture, sieve texture in plagioclases and also rapakivi texture are evidences of the magma mixing.