A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-Sand Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, Western Serbia

Item

Radosavljević, Slobodan

Recent mineralogical, chemical, physical, and crystallographic investigations of the Boranja orefield showed very complex mineral associations and assemblages where sulfosalts have significant role. The sulfosalts of the Boranja orefield can be divided in four main groups: (i) Pb-Sb(As)-S system with ±Fe and ±Cu; (ii) Cu(Ag)-Fe(Zn)-Sb(As)-S system; (iii) Ag(Pb)-Bi(Sb)-S; (iv) and Pb-Bi-S(Te) system. Spatially, these sulfosalts are widely spread, however, they are the most abundant in the following polymetallic deposits and ore zones: Cu(Bi)-FeS Kram-Mlakva; Pb(Ag)-Zn-FeS2 Veliki Majdan (Kolarica–Centralni revir–Kojići); Sb-Zn-Pb-As Rujevac; and Pb-Zn-FeS2-BaSO4 Bobija. The multi stage formation of minerals, from skarnhydrothermal to complex hydrothermal with various stages and sub-stages has been determined. All hydrothermal stages and sub-stages of various polymetallic deposits and ore zones within the Boranja orefield are followed by a variety of sulfosalts.

Цитирање: Radosavljević, Slobodan et al., “A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-Sand Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, Western Serbia” у Geološki anali Balkanskoga poluostrva(77).

Creator

sr Radosavljević, Slobodan
sr Stojanović, Jovica
sr Pačevski, Aleksandar
sr Radosavljević-Mihajlović, Ana
sr Kašić, Vladan

Date

sr 2016

Identifier

sr 10.2298/GABP1677001R

Publisher

sr Rudarsko-geološki fakultet Univerziteta u Beogradu

Source

sr Geološki anali Balkanskoga poluostrva

Subject

sr sulfosalts
sr Boranja orefield
sr West Serbia

Abstract

sr Recent mineralogical, chemical, physical, and crystallographic investigations of the Boranja orefield showed very complex mineral associations and assemblages where sulfosalts have significant role. The sulfosalts of the Boranja orefield can be divided in four main groups: (i) Pb-Sb(As)-S system with ±Fe and ±Cu; (ii) Cu(Ag)-Fe(Zn)-Sb(As)-S system; (iii) Ag(Pb)-Bi(Sb)-S; (iv) and Pb-Bi-S(Te) system. Spatially, these sulfosalts are widely spread, however, they are the most abundant in the following polymetallic deposits and ore zones: Cu(Bi)-FeS Kram-Mlakva; Pb(Ag)-Zn-FeS2 Veliki Majdan (Kolarica–Centralni revir–Kojići); Sb-Zn-Pb-As Rujevac; and Pb-Zn-FeS2-BaSO4 Bobija. The multi stage formation of minerals, from skarnhydrothermal to complex hydrothermal with various stages and sub-stages has been determined. All hydrothermal stages and sub-stages of various polymetallic deposits and ore zones within the Boranja orefield are followed by a variety of sulfosalts.

Date Available

sr 1

Date Created

sr 12

Date Accepted

sr NULL

Date Copyrighted

sr 2

Date Submitted

sr NULL

Date Issued

sr 77

Spatial Coverage

sr Beograd

Provenance

sr č292

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