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Original scientific paper
UDC: 552.321:[548/549:549.67 (497.6 Srebrenica)
DOI: 10.7251/afts.2014.0611.001R
COBISS.RS-ID 4570904

 

SREBRENICA OREFIELD, PODRINJE METALLOGENIC DISTRICT, REPUBLIC OF SRPSKA, B&H: HYDRATED Fe(Al)-PHOSPHATES AND THEIR PARAGENESES WITHIN THE Pb-Zn MINERALIZATION

 

Radosavljević Slobodan1, Đorđević Dragoslav1, Stojanović Jovica1, Radosavljević-Mihajlović Ana1, Kašić Vladan1
1Institute for Technology of Nuclear and Other Mineral Raw Materials,
Applied Mineralogy Unit, Belgrade, E. mail: Ova adresa el. pošte zaštićena je od spam napada, treba omogućiti JavaSkript da biste je videli

 

ABSTRACT  Full text (pdf)

The Srebrenica orefield is mostly composed of Tertiary dacite-andesites, and quartz latites, pyroclastites, Paleozoic schists, and Quaternary sediments, but in a in a lesser extent. The latest research showed that in the Srebrenica orefield occur complex mineral parageneses and associations deposited in pneumatolytic-hydrothermal and hydrothermal (from high- to low-temperature) stage, accompanied with very rare minerals. Beside ore mineral parageneses and associations, specials emphasis was on rare hydrated phosphates: vivianite, ludlamite, and vauxite. It is important to say that vauxite from the Srebrenica orefield is fourth discovery in the world. The minerals above were studied using DTA-TGA, IR-spectroscopy, and XRPD.

Key words: vivianite, ludlamite, vauxite, mineralogy, Srebrenica orefield, Republic of Srpska

 

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