×
Home Current Archive Editorial board
Instructions for papers
For Authors Aim & Scope Contact
Original scientific article

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.

References

1.
Đorđević R, D. Mineraloško ispitivanje ludlmita i vivijanita iz rudnika SaseSrebrenica. Novi Sad. 14 kongres geologa Srbije i Crne Gore sa sa međunarodnim učešćem. Knjiga apstrakata. 2005;21–2.
2.
A.M. K, Fontan PA, F. The phosphate mineral associations of the Tsaobismund pegmatite, Nambia. Contributions to Mineralogy and Petrology. 1986;92:502–17.
3.
J.W. The Mineralogy, Geochemistry and Phosphate Paragenesis of the Plaermo #2 Pegmatite, North Groton, New Hampshire. University of New Orleans, Thesis and Disertations, Paper. 2006;398.
4.
W.H., Rao BR. The crystal structure and the chemical composition of vauxite. American Mineralogist. 1968;53:1025–8.
5.
T. K, U., Stojanović J. Crystal structure and hydrogen bonding in vauxite, Fe2+Al2(PO4)2(OH)2•6H2O from Vitlovac locality, Bosnia and Herzegovina. In: Joint Meeting of the DGK, DMG and ÖMG. 2011. p. 136.

Citation

This is an open access article distributed under the  Creative Commons Attribution Non-Commercial License (CC BY-NC) License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. 

Article metrics

Google scholar: See link

The statements, opinions and data contained in the journal are solely those of the individual authors and contributors and not of the publisher and the editor(s). We stay neutral with regard to jurisdictional claims in published maps and institutional affiliations.