Pregled bibliografske jedinice broj: 851730
GEOCHEMICAL AND MINERALOGICAL CHARACTERISTICS OF THE CENTRAL PART OF THE ALŠAR DEPOSIT (REPUBLIC OF MACEDONIA) WITH PARTICULAR REFERENCE TO INVESTIGATIONS BY X-RAY DIFFRACTION
GEOCHEMICAL AND MINERALOGICAL CHARACTERISTICS OF THE CENTRAL PART OF THE ALŠAR DEPOSIT (REPUBLIC OF MACEDONIA) WITH PARTICULAR REFERENCE TO INVESTIGATIONS BY X-RAY DIFFRACTION // Geologica Macedonica, 30 (2016), 2; 115-127 (podatak o recenziji nije dostupan, članak, znanstveni)
CROSBI ID: 851730 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
GEOCHEMICAL AND MINERALOGICAL CHARACTERISTICS OF THE CENTRAL PART OF THE ALŠAR DEPOSIT (REPUBLIC OF MACEDONIA) WITH PARTICULAR REFERENCE TO INVESTIGATIONS BY X-RAY DIFFRACTION
Autori
Boev, Blažo ; Šorša, Ajka ; Boev, Ivan
Izvornik
Geologica Macedonica (0352-1206) 30
(2016), 2;
115-127
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
XRF-diffraction; rebulite; marcasite; quartz; gizmondine; vrbaite; Alšar
Sažetak
The Alšar deposit consists of several ore bodies and numerous occurrences, each characterized by specific associations of metal and mineral assemblages. The antimony-arsenic-thallium-gold mineralization occurs within a zone almost 3 km long and 200 – 300 m wide. Sb and gold dominate the central part of the deposit, but it also contains significant amounts of arsenic, thallium, minor barium, mercury and traces of lead. The ore bodies contain 2 to 3% antimony, 2% arsenic, up to 0.4% thallium, up to 3.5 ppm gold and 435 ppm barium. In this paper geochemical and mineralogical characteristics of the central part of the Alšar deposit are presented along with the results of new investigations of some specimens from this area.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
