That part of the Serbia is
characterized by the presence of numerous lead, zinc and at lesser amount
copper beds and outcrops accompanying precious metals. Initiating by the Roman
times, the mining activities at the area ranges its maximum level at Middle
Ages previously and at twentieth century lately, The mentioned metallogenic
belt usually is in accordance with the Vardar zone, the predominant tectonic unit
and the lead-zinc beds and exposures picture a Avala, Kosmaj, Rudnik. Kotlenik.
Tolisnica and Stanca (near Goc), Kopaonik (Sastavci, Kizevak, Plavkovo. Belo
Brdo, Crnac. Koporic, Stari Trg and etc), Novo Brdo and Radan Mountains (Lece.
Draznja, Tulare, Sijarinska Banja and others) lining up from north to south.
Precious metals either go along with lead, zinc and copper and antimony,
arsenite and quartz at a lesser degree or in lycvenites and diabase and dacite
andesite at a lesser amount in the form of native as well. Mineralization
patterns are veins, disseminated bodies and sometimes mesh.
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Şubat 1999 |
Yayımlandığı Sayı | Yıl 1999 Cilt: 121 Sayı: 121 |
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