Fluids in Quartz form Central Bosnia, Indicators of Alpine Retrogressive Metamorphism (CROSBI ID 480942)
Prilog sa skupa u zborniku | sažetak izlaganja sa skupa | međunarodna recenzija
Podaci o odgovornosti
Palinkaš, Ladislav ; Pavlović, Gordana ; Jurković, Ivan ; Hrvatović, Hazim
engleski
Fluids in Quartz form Central Bosnia, Indicators of Alpine Retrogressive Metamorphism
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.
fluid inclusion; quartz; metamorphism; Busovača; Čemernica; Bosnia and Herzegovina
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Podaci o prilogu
23-25-x.
1999.
objavljeno
Podaci o matičnoj publikaciji
II. Field Meeting of Carpathian-Balkan Association
Faryad, S. W.
Košice: Department of Geology and Mineralogy F BERG , Technical Universi
Podaci o skupu
II. Field Meeting of Carpathian-Balkan Association
poster
31.05.1999-05.06.1999
Košice, Slovačka