Pregled bibliografske jedinice broj: 197483
Identification of nesosilicate minerals from Macedonia by powder XRD and vibrational spectroscopy
Identification of nesosilicate minerals from Macedonia by powder XRD and vibrational spectroscopy // XIVth Croatina-slovenian Crystallographic Meeting, Book of Abstracts / Popović, Stanko (ur.).
Zagreb: Hrvatska kristalografska zajednica HAZU, 2005. str. 38-38 (predavanje, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 197483 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Identification of nesosilicate minerals from
Macedonia by powder XRD and vibrational spectroscopy
Autori
Jovanovski, Gligor ; Kaitner, Branko ; Makreski, Petre ; Boev, Boev ; Stojančeska, Stojanka
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
XIVth Croatina-slovenian Crystallographic Meeting, Book of Abstracts
/ Popović, Stanko - Zagreb : Hrvatska kristalografska zajednica HAZU, 2005, 38-38
Skup
XIVth Croatinan-Slovenian Crystallographic Meeting
Mjesto i datum
Vrsar, Hrvatska, 15.06.2005. - 17.06.2005
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Macedonia ; minerals ; nesosilicates ; powder diffraction ; vibrational spectroscopy
Sažetak
The powder XRD and vibrational (infrared and Raman) spectroscopy are used for identification of seven common nesosilicate minerals from the Republic of Macedonia: almandine, Fe3Al2(SiO4)3 ; spessartine, Mn3Al2(SiO4)3 ; zircon, ZrSiO4 ; titanite, CaTiSiO5 ; olivine, (Mg, Fe)2SiO4 ; staurolite, Fe2Al9O6(SiO4)4(OH)2 and kyanite, Al2SiO5. The identification is based on the comparison of their powder XRD patterns and vibrational spectra with the corresponding XRD, FTIR and Raman literature data for the analogue mineral species originating all over the world. In general, rather expressed similarity among the infrared spectra of the minerals are observed being mainly due to their common structural characteristics. The similarity is especially expressed in the case of the isomorphous almandine and spessartine which form solid solution. The similarity between the Raman spectra of the studied minerals is less expressed compared to the IR analogues. The difficulties appeared in the process of the identification of staurolite and olivine (forsterite or fayalite) specimens related to the lower quality of their Raman spectra are outrun by use of their powder XRD patterns.
Izvorni jezik
Engleski
Znanstvena područja
Kemija
POVEZANOST RADA
Projekti:
0119630
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Branko Kaitner
(autor)