id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
ggj-1660	Tsutsunava, Tamara; Beridze, Giorgi; Javakhishvili, Irakli	On Some Accessory Minerals in Upper Paleozoic Granites of the Khrami Crystalline Massif	2023	7	.pdf	application/pdf	2739	168	52	The core of the garnet was formed in the magmatic stage, in paragenesis Bt+Pl+Or+Grt+Qz, but its periphery - in the cooling stage of granite magma, in paragenesis - Ab+Mc+Grt+Qz±Ms. • The genesis of allanite in the biotite-hornblende-allanite bearing granites of the massif is due to the concentration of REE in the granite magma and the introduction of calcium by hydrothermal solutions. • Allanites of biotite-hornblende-allanite bearing granites from the Khrami crystalline massif belong to the cerium variety with high Ce2O3, La2O3 and Nd2O3. Although allanite is generally an accessory mineral, it is a rock-forming mineral in biotite- hornblende-allanite bearing granites of the Khrami crystalline massif	cache/ggj-1660.pdf	txt/ggj-1660.txt