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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

Balen, Dražen ; Petrinec, Zorica ; Juranić, Valentina Infrared study of O-H stretching region in the nodular and disseminated dravite-schorl series tourmalines from Moslavačka gora (Croatia) // Abstracts book / Horvat, Marija ; Wacha, Lara (ur.). Zagreb: Hrvatski geološki institut, 2015. str. 22-23

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

Povezanost rada

nije evidentirano