Hostname: page-component-586b7cd67f-2brh9 Total loading time: 0 Render date: 2024-11-22T19:37:03.778Z Has data issue: false hasContentIssue false

Dickite and kaolinite in the Pb-Zn-Ag sulphide deposits of northern Kosovo (Trepča and Crnac)

Published online by Cambridge University Press:  09 July 2018

S. S. Palinkaš*
Affiliation:
Faculty of Science, Horvatovac bb, HR-10000 Zagreb, Croatia
S. B. Šoštarić
Affiliation:
Faculty of Science, Horvatovac bb, HR-10000 Zagreb, Croatia
V. Bermanec
Affiliation:
Faculty of Science, Horvatovac bb, HR-10000 Zagreb, Croatia
L. Palinkaš
Affiliation:
Faculty of Science, Horvatovac bb, HR-10000 Zagreb, Croatia
W. Prochaska
Affiliation:
Montanuniversität Leoben, Peter-Tunner-Straße 5, 8700 Leoben, Austria
K. Furić
Affiliation:
Ruđer Bošković Institute, Bijenička 54, P.O.B. 180, HR-10000 Zagreb, Croatia
J. Smajlović
Affiliation:
Geotechnical Faculty Varaždin, Hallerova aleja 7, HR-42000 Varaždin, Croatia
*

Abstract

Alteration minerals dickite and kaolinite were detected in two hydrothermal Pb-Zn-Ag sulphide deposits in the northern Kosovo region. Dickite is associated with skarn mineralization in the Trepča (Stari Trg) deposit and kaolinite occurs in vein sulphide parageneses in the Crnac deposit. The mineralogical characteristics of dickite and kaolinite were determined by X-ray powder diffraction, Raman spectroscopy and scanning electron microscopy with EDS detector. Fluid-inclusion microthermometry and ion chromatography of leachates provided information on the P-T-X conditions of the genesis of dickite at Trepča. It was formed at temperatures between 290 and 330ºC and pressures between 12 and 60 MPa from a fluid with salinity in the range 6–8.5 wt.% NaCl eq. and pH <5.5. Kaolinite was deposited from a fluid with minimum temperatures between 210 and 250ºC, minimum pressure of 1.7 to 3.7 MPa, and salinity between 4.6 and 5.1 wt.% NaCl eq. Both dickite and kaolinite are related to the acidic pre-mineralization phase in the deposits.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2009

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Bailey, S.W. & Tyler, S.A. (1960) Clay minerals associated with the Lake Superior iron ores. Economic Geology, 55, 150175.Google Scholar
Bakker, R.J. (2003) Package FLUIDS 1. Computer programs for analysis of fluid inclusion data and for modelling bulk fluid properties. Chemical Geology, 194, 323.CrossRefGoogle Scholar
Balan, E., Saitta, A.M., Mauri, F. & Calas, G. (2001) Firstprinciples modeling of the infra-red spectrum of kaolinite. American Mineralogist, 86, 13211330.CrossRefGoogle Scholar
Balan, E., Lazzeri, M., Saitta, A.M., Allard, T., Fuchs, Y. & Mauri, F. (2005) First-principles study of OHstretching modes in kaolinite, dickite, and nacrite. American Mineralogist, 90, 5060.CrossRefGoogle Scholar
Bish, D.L. (1993) Rietveld refinement of the kaolinite structure at 1.5 K. Clays and Clay Minerals, 41, 738744.Google Scholar
Bogdanović, P., Urošević, M., Urošević, D., Dimitrijević, M., Marković, B., Pavić, A., Menković, L. & Folgić, K. (1978) General geological map of SFRJ 1:100 000, schist Titova Mitrovica. Federal Geological Survey, Belgrade.Google Scholar
Brindley, G.W. & Brown, G. (1980) Crystal Structures of Clay Minerals and their X-ray Identification. Monograph 5, Mineralogical Society, London.Google Scholar
Brindley, G.W. & Porter, A.R.D. (1978) Occurrence of dickite in Jamaica. Ordered and disordered varieties. American Mineralogist, 63, 554562.Google Scholar
Browne, P.R.L. (1978) Hydrothermal alteration in active geothermal fields. Annual Review of Earth and Planetary Sciences, 6, 229250.Google Scholar
Buatier, M.D., Potdevin, J.-L., Lopez, M. & Petit, S. (1996) Occurrence of nacrite in the Lodève Permian basin (France). European Journal of Mineralogy, 8, 847852.Google Scholar
Can, I. (2002) A new improved Na/K geothermometer by artificial neural networks. Geothermics, 31, 751760.CrossRefGoogle Scholar
Chen, P.Y., Wang, M.K. & Yang, D.S. (2001) Mineralogy of dickite and nacrite from northern Taiwan. Clays and Clay Minerals, 49, 586595.Google Scholar
Corbett, G.J. & Leach, T.M. (1998) Controls on hydrothermal alteration and mineralization. Pp. 6982 in: Southwest Pacific Rim Gold-Copper Systems: Structure, Alteration, and Mineralization (Corbett, G.J. and Leach, T.M., editors). Special Publication, 6, Society of Economic Geologists, Tulsa, Oklahoma, USA.Google Scholar
Cvetković, V., Prelević, D., Downes, H., Jovanović, M., Vaselli, O. & Pecskay, Z. (2004) Origin and geodynamic significance of Tertiary postcollisional basaltic magmatism in Serbia (central Balkan Peninsula). Lithos, 73, 161186.Google Scholar
Dimitrijević, M.D. (1997) Geology of Yugoslavia. Geological Institute GEMINI Special Publication, Belgrade.Google Scholar
Fialips, C.-I., Majzlan, J., Beaufort, D. & Navrotsky, A. (2003) New thermochemical evidence on the stability of dickite vs. kaolinite. American Mineralogist, 88, 837845.Google Scholar
Forgan, C.B. (1950) Ore deposits at the Stari Trg leadzinc mine. Pp. 290307 in: 18th International Geological Congress, London, Part VII, Symposium of Section F (Dunham, K.C., editor).Google Scholar
Fournier, R.O. & Truesdell, A.H. (1973) An empirical Na—K—Ca geothermometer for natural waters. Geochimica et Cosmochimica Acta, 37, 12551273.CrossRefGoogle Scholar
Helgeson, H.C. & Kirkham, D.H. (1974) Theoretical prediction of the thermodynamic behavior of aqueous electrolytes at high pressures and temperatures; I. Summary of the thermodynamic/electrostatic properties of the solvent. American Journal of Science, 274, 10891198.CrossRefGoogle Scholar
Helgeson, H.C., Delany, J.M., Nesbitt, H.W. & Bird, D.K. (1978) Summary and critique of the thermodynamic properties of rock-forming minerals. American Journal of Science, 278-A, 1229.Google Scholar
Helgeson, H.C., Kirkham, D.H. & Flowers, G.C. (1981) Theoretical prediction of the thermodynamic behavior of aqueous electrolytes at high pressures and temperatures. IV. Calculation of activity coefficients, osmotic coefficients and apparent molal and standard and relative partial molal properties to 600°C and 5 kbar. American Journal of Science, 281, 12491516.Google Scholar
Henley, R.W., Truesdell, A.H. & Barton, P.B. (1984) Fluid-mineral equilibria in hydrothermal systems. Reviews in Economic Geology, 1, 1267.Google Scholar
Johnson, C.T., Helsen, J., Schoonheydt, R.A., Bish, D.L. & Agnew, S.F. (1998) Single-crystal Raman spectroscopic study of dickite. American Mineralogist, 83, 7584.Google Scholar
Miletić, G. (1995) The structure of the lead and zinc deposit at Crnac (in Serbian with English summary). Pp. 299304 in: Geology and Metallogeny of the Kopaonik Mt. Symposium, Kopaonik, Belgrade.Google Scholar
Murray, H.H. (1988) Kaolin minerals: their genesis and occurrences. Pp. 6789 in: Hydrous Pyllosilicates (exclusive of micas) (Bailey, S.W., editor). Reviews in Mineralogy, 19, Mineralogical Society of America, Washington, D.C. CrossRefGoogle Scholar
Nesbitt, B.E. & Prochaska, W. (1998) Solute chemistry of inclusion fluids from sparry dolomites and magnesites in Middle Cambrian carbonate rocks of the southern Canadian Rocky Mountains. Canadian Journal of Earth Sciences, 35, 546555.Google Scholar
Pavlović, S. & Todorović, Ž. (1961) Sulphide miner-alisation and Pb-Zn ore types at Rogozna Mt. (in Serbian). Glas CCXLV, 21, 104105, Belgrade.Google Scholar
Pitzer, K.S. (1991) Ion interaction approach: theory and data correlation. Pp. 76153 in: Activity Coefficient in Electrolyte Solutions (Pitzer, K.S., editor). CRC Press, Boca Raton, Florida, USA.Google Scholar
Schumacher, F. (1954) The ore deposits of Yugoslavia and the development of its mining industry. Economic Geology, 49, 451492.CrossRefGoogle Scholar
Urošević, M., Pavlović, Z., Klisić, M., Brkulović, T., Malešević, M. & Trifunović, S. (1966) General geological map of SFRJ 1:100 000, sheet Novi Pazar. Federal Geological Survey, Belgrade.Google Scholar
Wiewióra, A., Wieckowski, T. & Sokolowska, A. (1979) The Raman spectra of kaolinite sub-group minerals and of pyrophyllite. American Mineralogist, 35, 514.Google Scholar
Zhang, Y.G. & Frantz, J.D. (1987) Determination of the homogenization temperatures and densities of super-critical fluids in the system NaCl-KCl-CaCl2-H2O using synthetic fluid inclusions. Chemical Geology, 64, 335350.Google Scholar
Zotov, A., Mukhamet-Galeev, A. & Schott, J. (1998) An experimental study of kaolinite and dickite relative stability at 150-300°C and the thermodynamic properties of dickite. American Mineralogist, 83, 516524.CrossRefGoogle Scholar