granitoids of the Loki Crystalline Massif

The Loki crystalline massif is the inlier of the pre-Alpine substrate of the Somkhit-Karabakh tectonic zone and belongs to the Beiburt-Sevanian terrane. Loki crystal massif is built by allochthonous metamorphic complex and magmatites of different age and composition. Granitoids are the subject of our research, in particular, Upper Devonian gneiss-like quartz diorites and Late Variscan granites. Petrological and geochemical data of the aforementioned granitoids will be considered in the report.