Pregled bibliografske jedinice broj: 184913
Carbon and oxygen isotope composition of the Dinaridic ophiolite related magnesites
Carbon and oxygen isotope composition of the Dinaridic ophiolite related magnesites // Mineral Exporation and Sustainable Development (SGA) / Demetrios G. Eliopoulos et al. (ur.).
Atena: Millpress Rotterdam, 2003. str. 24-28 (poster, međunarodna recenzija, sažetak, znanstveni)
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Naslov
Carbon and oxygen isotope composition of the Dinaridic ophiolite related magnesites
Autori
Jurković, Ivan ; Pamić, Jakob
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Mineral Exporation and Sustainable Development (SGA)
/ Demetrios G. Eliopoulos et al. - Atena : Millpress Rotterdam, 2003, 24-28
Skup
Proceedings of the seventh biennal SGA meeting Athens / Greece
Mjesto i datum
Atena, Grčka, 24.08.2003. - 28.08.2003
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Dinarides; magnesite deposits; carbon and oxygen isotope composition; comparison with world magnesites
Sažetak
The Dinaridic ophiolite related magnesites have averages of 13C and 18O of +1.3 vs. +26.1 ‰ for the Late Jurassic contactmetamorphic-type 12.2 vs. +26.4 ‰ for the Oligocene vein magnesites 8.8 vs. +27.7 ‰ for stockwork deposits ; -1.1 vs. +31.5 ‰ for Miocene detrital magnesites ; and +1.7 vs. +32.8 ‰ for Miocene Bela Stena sedimentary deposits. Authors compared carbon and oxygen isotope composition of ophiolite related Dinaridic and world known magnesites. Comparison pointed out the identical span of values for the vein and stockwork types and some differences, but still with the similar trend at sedimentary magnesite deposits.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
