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[en] Garnets have a great petrogenetic significance, because their composition depends on the chemical composition of source rocks and the pressure and temperature under which they crystallize. For that reason garnet is usually used as an important agent of provenance and history of rocks. The present study is focused on garnet recovered from volcanoclastic infillings of maars and diatremes of the South Slovakian alkali basalt volcanic field. Chemical composition and contained inclusions of metamorphic garnets are consistent with the garnets of higher metamorphic facies (metapelites, metabasites). We assume that garnets possibly originate from presumed gneiss-amphibolite basement complex of Cerova Highlands. Primary igneous garnets possibly crystallized from alkaline basaltic magma or have been derived from underlying granitoids. (authors)
Source
Galambos, M. (Department of Inorganic Chemistry, Faculty of Natural Sciences, Comenius University, Bratislava (Slovakia)); Dzugasova, V.; Sevcovicova, A. (Department of Genetics, Faculty of Natural Sciences, Comenius University, Bratislava (Slovakia)) (eds.); Faculty of Natural Sciences, Comenius University, Bratislava (Slovakia); 1741 p; ISBN 978-80-223-3859-2; 
; 30 May 2015; p. 1302-1307; Student Scientific Conference PriF UK 2015; Studentska vedecka konferencia PriF UK 2015; Bratislava (Slovakia); 22 Apr 2015; PROJECT VEGA 2/0069/13; Also available from https://fns.uniba.sk/studium/svk/zborniky-svk/; 1 map, 2 figs., 18 refs.
; 30 May 2015; p. 1302-1307; Student Scientific Conference PriF UK 2015; Studentska vedecka konferencia PriF UK 2015; Bratislava (Slovakia); 22 Apr 2015; PROJECT VEGA 2/0069/13; Also available from https://fns.uniba.sk/studium/svk/zborniky-svk/; 1 map, 2 figs., 18 refs.