Pregled bibliografske jedinice broj: 402266
Raman spectra and luminescence of the minerals with aeschynite and euxenite crystal structure
Raman spectra and luminescence of the minerals with aeschynite and euxenite crystal structure // EUCMOS 2008 XXXIX European Congress on Molecular Spectroscopy, Book of Abstracts / Musić, Svetozar ; Ristić, Mira ; Krehula, Stjepko (ur.).
Zagreb: Institut Ruđer Bošković, 2008. str. 267-267 (poster, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 402266 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Raman spectra and luminescence of the minerals with aeschynite and euxenite crystal structure
Autori
Tomašić, Nenad ; Gajović, Andreja ; Bermanec, Vladimir
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
EUCMOS 2008 XXXIX European Congress on Molecular Spectroscopy, Book of Abstracts
/ Musić, Svetozar ; Ristić, Mira ; Krehula, Stjepko - Zagreb : Institut Ruđer Bošković, 2008, 267-267
Skup
EUCMOS 2008 XXXIX European Congress on Molecular Spectroscopy
Mjesto i datum
Opatija, Hrvatska, 31.08.2008. - 05.09.2008
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
aeschynite; euxenite; Raman spectra; luminescence
Sažetak
Metamict minerals aeschynite-(Y) and polycrase-(Y) showed aeschynite and euxenite structure after recrystallization, respectively. Raman spectra of these minerals show luminescence lines strongly interfering with normal vibration modes (Fig. 1), especially in 200-500 cm-1 range (region of Ti/Nb/Ta-O stretching and bending modes). However, their synthetic analogs of REETiTaO6 composition having single REE content and aeschynite or euxenite structure do not show luminescence lines using 488 and 514.5 nm Ar excitation lines up to 900 cm-1 with exception of the Er member [1]. In the case of polycrase-(Y) a separated strong luminescence line is also observed at 684 cm-1. The origin of luminescence in these minerals is discussed in term of the complex REE composition, the crystal field formed in the structure during recrystallization process and its influence on REE in cation sites.
Izvorni jezik
Engleski
Znanstvena područja
Fizika, Geologija
POVEZANOST RADA
Projekti:
098-0982904-2898 - Fizika i primjena nanostruktura i volumne tvari (Ivanda, Mile, MZOS ) ( CroRIS)
119-0000000-1158 - Međudjelovanje minerala i okoliša (Bermanec, Vladimir, MZOS ) ( CroRIS)
Ustanove:
Institut "Ruđer Bošković", Zagreb,
Prirodoslovno-matematički fakultet, Zagreb