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Petrographic characteristics and geochimstry in the part of Gjilani Region – Kosova

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EN
Abstrakty
EN
The country of the Republic of Kosovo is situated in the central part of the Balkan Peninsula. In the Southwest, it is bordered by Albania, in the West by Montenegro, in the North and East by Serbia and in the Southeast by North Macedonia. In this scientific paper was done the identification detailed for rocks found on the researched region. it was done the identification detailed for rocks found in the researched region. The region research it’s done scale by 1:25 000 for comparison map of geology scale by 1:200 000 and paper will be treated the mineralogical content, petrography microscope preparation, and geochemistry. For the region of Gjilan, the analysis was performed: for large elements, for small elements and traces, and for rare soils. The processing of the analysis of large elements, traces, and sub-traces was performed in the geochemical-petrological software MINPET. Constructed diagrams show that we are dealing with rocks generated in differentiated geodynamic environments. Most of the rocks analyzed fall in the field of basic and acid rocks, and only a small part of them belong to the medium and ultrabasic rocks. Acid rocks are represented mainly by their Metamorphism types – gneiss and less of those ages with them younger – granite. They generally show geochemical features of volcanic type than orogenic in acid magmatism The purpose of the paper it the proposal of the paper is the identification rocks in the exploration zone for the preparation petrographic of microscope and processing of the analysis of large elements, traces, and sub-traces was performed in the geochemical-petrological software MINPET. It was done by the evidencing and detailed description of all the types of rocks found in the researched region. The samples were taken from those rocks for the preparation of petrography microscope preparation. The analyses were completed at the certified laboratory of Geology-Mining Faculty (Polytechnic University of Tirana) – Geosciences Institute.
Czasopismo
Rocznik
Tom
Strony
217--232
Opis fizyczny
Bibliogr. 19 poz., rys.
Twórcy
  • Faculty of Geoscience, University of Mitrovica "Isa Boletini"
Bibliografia
  • [1] KUTLLOVCI F., Petrological aspects of the metamorphic complex of Dardana area (Gjilan–Kamenica region), Ph.D. thesis.
  • [2] KUTLLOVCI F., 2021, Structure and Metamorphism of the Dardania Zone in the Eastern Part of Gjilan Region (Kosove), Mining Science, 28, 93–102.
  • [3] KUTLLOVCI F., 2018, Petrographic Characteristics of the North-Western Part of Kosovo, Vol. 25.
  • [4] MESHI A., FEJZA I., MUCEKU B., MEHA M., 2010, Explanatory text of the geological-structural mapping scale 1:25 000 for Gjilan region, ICMM internal report, Pristina, Kosovo, 54f.
  • [5] DALLMEYER R.D., NEUBAUER F., HANDLER R., FRITZ H., MÜLLER W., PANA D., PUTIS M., 1996, Tectonothermal evolution of the Alps and Carpathians: Evidence from 40Ar/39Ar mineral and whole rock data, Eclogae Geologicae Helvetiae, 89, 203–227.
  • [6] KRSTIĆ B., KARAMATA S., MILIĆEVIĆ V., 1996, The Carpatho-Balkanide terranes a correla tion. [In:] V. Knežević, B. Krstić B. (Eds.), Terranes of Serbia, Faculty of Mining and Geology, Belgrade, 71–76.
  • [7] HAYDOUTOV I., JANEV S., 1996, The Proto-Moesian continent of the Balkan Peninsula – a peri-Gondwanaland piece, Tectonophysics, 272, 303–313.
  • [8] KARAMATA S., 2006, The geodynamical framework of the Balkan Peninsula: its origin due to the approach, collision and compression of Gondwanian and Eurasian units. [In:] A.H.F. Robertson, D. Mountrakis (Eds.), Tectonic Development of the Eastern Mediterranean Region, Geological Society, London, Special Publication, 260, 155–178.
  • [9] DERCOURT J., GAETANI M., VRIELYNCK B., BARRIER E., BIJU-DUVAL B., BRUNNET M.F., CADET J.P., CRASQUIN S., SANDULESCU M. (Eds.), 2000, Peri-Tethys Palaeogeographical Atlas, Gauthier-Villars, Paris.
  • [10] STAMPFLI G.M., BOREL G.D., 2000, The TRANSMED transect in space and time. Constraints on the Paleotectonic Evolution of the Mediterranean Domain. [In:] W. Cavazza, B. Roure, W. Spakman, G.M. Stampfli, P.A. Ziegler (Eds.), 2000, The TRANSMED Atlas. The Mediterranean Region from Crust to Mantle, Springer, Berlin–Heidelberg, 53–90.
  • [11] STAMPFLI G., MOSAR J., FAURE P., PILLEVUIT A., VANNAY J.-C., 2001, Permo-Mesozoic evolution of the western Tethys realm: the Neotethys East Mediterranean basin connection. [In:] P. Ziegler, W. Cavazza, A.H.F. Robertson, S. Crasquin-Soleau (Eds.), 2001, Peri-Tethys Memoir 5, Peri-Tethys Rift/Wrench Basins and Passive Margins, Memoirs du Museum National d’Histoire Naturelle, 51–108.
  • [12] SCHMID S.M., BERNOULLI D., FÜGENSCHUH B., MATENCO L., SCHEFER S., SCHUSTER R., TISCHLER M., USTASZEWSKI K., 2008, The Alpine-Carpathian-Dinaridic orogenie system: correlation and evolution of tectonic units, Swiss Journal of Geosciences, pp. 1–48.
  • [13] KOSSMAT F., Geologie der zentralen Balkan Kriegsschauplätze 1914–1918, Geologisch Dargstellt, Vol. 12, Berlin 1924, 198 pp.
  • [14] MERCIER J., 1968, Contibution a l`étude du métamorphisme et l`évolution magmatique des zones internes des Hellénides, Annales géologiques des pays helléniques, T. XX, 599–792.
  • [15] KOCKEL F., Mollat H., Walther H.W., 1977, Erlaeuterungen zur Geologischen Karte der Chalkidhiki und angrenzender Gebiete, 1:100 000 (Nord-Griechenland), Bundesanst. fuer Geowiss. und Rohst. Hanover, Federal Republic of Germany, pp. 119, 1973.
  • [16] AUBOUIN J., BONNEAU M., DAVIDSON J., LEBOULENGER P., MATESCO S., ZAMBETAKIS A., 1976, Esquisse structurale de l`Arc égéen externe des Dinarides aux Taurides, Bulletin de la Société Géologique de France, 7/2, 327–336.
  • [17] JACOBSHAGEN V., 1986, Geologie von Griechenland, Beiträge zur regionalen Geologie der Erde, 19, Geb. Bornträger, p. 363.
  • [18] Anonim, 1974, Harta gjeologo-tektonike e Kosovës ne shkallë 1:100 000, Zagreb, pp. 225.
  • [19] MOUTRAKIS D., 1986, The Pelagonian Zone in Greece: a polyphase-deformed fragment of the Cirnrnerian continent and its role in the geotectonic evolution of the eastern Mediterranean, Journal of Geology, Vol. 94, pp. 335–347.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-85f20f0f-36a3-49f4-8706-cb64328799e9
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