Naslov
Fluids in Quartz form Central Bosnia, Indicators of Alpine Retrogressive Metamorphism

Autori
Palinkaš, Ladislav ; Pavlović, Gordana ; Jurković, Ivan ; Hrvatović, Hazim

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni

Izvornik
II. Field Meeting of Carpathian-Balkan Association / Faryad, S. W. - Košice : Department of Geology and Mineralogy F BERG , Technical Universi, 1999, 23-25

Skup
II. Field Meeting of Carpathian-Balkan Association

Mjesto i datum
Košice, Slovačka, 31.05.1999. - 05.06.1999

Vrsta sudjelovanja
Poster

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
fluid inclusion; quartz; metamorphism; Busovača; Čemernica; Bosnia and Herzegovina

Sažetak
The fluid inclusion in the quartz from Čemernica mineralization are aqueous and aqueous carbonic in nature, Their P-T-X characteristics show a complex geological history of the area, which underwent poly-phase metamorphism. The P-T-t metamorphic loop, has characteristics of the regional metamorphism caused collisional processes. Isochores of the aqueous FI-s were calculated by ZHANG and FRANTZ (1987) equation of state using FLINCOR 1.4 Version (BROWN, 1989). Some selected H2O-NaCl-CO2 FI-s with Tm CO2 close to -57 oC (approaching CO2 triple point) were elaborated by Bowers and Helgeson (1983) EOS. They intersect the retrogressive part of the P-T loop. Similar FI-s have been already found and determined in quartz and hyalophane within chloritoide schists of the Busovača area, adjacent to the Čemernica mineralisation.

Izvorni jezik
Engleski

Znanstvena područja
Geologija

POVEZANOST RADA