Pregled bibliografske jedinice broj: 61069
Sulphur isotope and fluid inclusion data of barites from the Dinarides
Sulphur isotope and fluid inclusion data of barites from the Dinarides // Mineral Deposits: Processes to Processing / Stanley et al. (ur.).
Rotterdam : Boston (MA) : Taipei: A.A. Balkema Publishers, 1999. str. 45-48
CROSBI ID: 61069 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Sulphur isotope and fluid inclusion data of barites from the Dinarides
Autori
Jurković, Ivan ; Palinkaš, Ladislav A.
Vrsta, podvrsta i kategorija rada
Poglavlja u knjigama, znanstveni
Knjiga
Mineral Deposits: Processes to Processing
Urednik/ci
Stanley et al.
Izdavač
A.A. Balkema Publishers
Grad
Rotterdam : Boston (MA) : Taipei
Godina
1999
Raspon stranica
45-48
ISBN
90 5809 068x
Ključne riječi
sulphur isotope, fluid inclusion, barite, Dinarides
Sažetak
Barite deposits of the Dinarides occur within a Paleozoic and Triassic nappe. Barites, genetically related to Upper Paleozoic rhyolites, are characterized by δ 34S +10.37� and with 3.62% SrSO4. Barites related to the Triassic Alpine rift magmatism have δ 34S +21.40� and 2.46% SrSO4. A fluid inclusion study of Variscan barite deposits proved the coexistence of Variscan, post-Variscan and Late Alpidic fluids in different proportions. Post-Variscan fluids are homogenous over thw whole Dinarides. similar characteristic features have been found in central and western Europe. Triassic barite deposits are characterized by low homogenization temperature and low salinity.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
