Infrared study of O-H stretching region in the nodular and disseminated dravite-schorl series tourmalines from Moslavačka gora (Croatia) (CROSBI ID 627810)
Prilog sa skupa u zborniku | sažetak izlaganja sa skupa | domaća recenzija
Podaci o odgovornosti
Balen, Dražen ; Petrinec, Zorica ; Juranić, Valentina
engleski
Infrared study of O-H stretching region in the nodular and disseminated dravite-schorl series tourmalines from Moslavačka gora (Croatia)
Origin of the nodular tourmaline, crystallized as the last mineral in the evolved granitic system of Moslavačka Gora Mt. has been attributed to the interaction of a fluid phase from the residual granitic melt with the wall-rock derived fluid in the environment of low pressure and relative rapid cooling, which resulted in increased MgO content. Disseminated tourmaline from the leucogranite host, on the other hand, can be considered as a typical magmatic (pegmatite) product and a common accessory phase. Such interpretation has been corroborated by the variation patterns in composition of the two tourmaline types and 3D tomographic study of tourmaline nodule shape and distribution.
IR spectra; tourmaline; dravite; schorl; Moslavačka Gora Mt.
Rad izrađen u sklopu projekta HRZZ IP-2014-09-9541
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Podaci o prilogu
22-23.
2015.
objavljeno
Podaci o matičnoj publikaciji
Abstracts book
Horvat, Marija ; Wacha, Lara
Zagreb: Hrvatski geološki institut
978-953-6907-50-2
Podaci o skupu
5.Hrvatski geološki kongres s međunarodnim sudjelovanjem
poster
01.01.2015-01.01.2015
Osijek, Hrvatska