Fluid Inclusions and K/Ar Dating of the Allšar Au-Sb-As-Tl Mineral deposit, Macedonia
AbstractThe Allšar Au-Sb-As-Tl mineral deposit, Macedonia, occurs in the southern part of the Vardar zone. The deposit carries Carlin-type of mineralization hosted by calcareous sedimentary complex. Mineral assemblages and alterations display characteristic zonal distribution. According to the fluid inclusion data, mineral deposition occurred as a result of cooling, dilution and neutralization of the ore-bearing fluids. Neogene magmatism (4.6 to 5.8 Ma) served as the heat source responsible for driving convective hydrothermal circulation at the Allšar deposit.
Apr 19, 2013
How to Cite
STRMIĆ PALINKAŠ, Sabina et al. Fluid Inclusions and K/Ar Dating of the Allšar Au-Sb-As-Tl Mineral deposit, Macedonia. Geologica Macedonica, [S.l.], v. 24, n. 1/2, p. pp.63-71, apr. 2013. ISSN 1857- 8586. Available at: <http://js.ugd.edu.mk/index.php/GEOLMAC/article/view/264>. Date accessed: 23 sep. 2019.