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

By
Slobodan Radosavljević ,
Slobodan Radosavljević
Contact Slobodan Radosavljević

Institute for Technology of Nuclear and Other Mineral Raw Materials, Applied Mineralogy Unit, Belgrade, Serbia

Dragoslav Đorđević ,
Dragoslav Đorđević

Institute for Technology of Nuclear and Other Mineral Raw Materials, Applied Mineralogy Unit, Belgrade, Serbia

Jovica Stojanović ,
Jovica Stojanović

Institute for Technology of Nuclear and Other Mineral Raw Materials, Applied Mineralogy Unit, Belgrade, Serbia

Ana Radosavljević-Mihajlović ,
Ana Radosavljević-Mihajlović

Institute for Technology of Nuclear and Other Mineral Raw Materials, Applied Mineralogy Unit, Belgrade, Serbia

Vladan Kašić
Vladan Kašić

Institute for Technology of Nuclear and Other Mineral Raw Materials, Applied Mineralogy Unit, Belgrade, Serbia

Abstract

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.

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