NEW DATA ON PETROGEOCHEMICAL RESEARCH OF PRE-ALPINE QUARTZ DIORITES AND GRANITOIDS OF THE LOKI CRYSTALLINE MASSIF (LESSER CAUCASUS)
DOI:
https://doi.org/10.52340/pajig.2024.136.02Keywords:
petrogeochemistry, pre-Alpine granitoids, the Lesser CaucasusAbstract
The issues of geochemistry and genesis of the Upper Devonian quartz diorites and Late Variscan granitoids of the pre-Alpine basement of the Loki crystalline massif are discussed. According to I, S and A types of the geochemical classification of granits, quartz diorites belong to S and partly M type granites, and granitoids belong to S and I types. The chemical composition of granitoids corresponds to normal, mostly normal alkaline-acid rocks. The granitoids and quartz diorites of the massif are characterized by the signs of magmatic rocks of volcanogenic-arc origin, which indicates mainly the subduction conditions of their formation.
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