{"id":765,"date":"2021-03-31T14:14:35","date_gmt":"2021-03-31T12:14:35","guid":{"rendered":"http:\/\/kmplg.sk\/?page_id=765"},"modified":"2021-08-25T09:06:06","modified_gmt":"2021-08-25T07:06:06","slug":"rndr-ondrej-nemec-phd-2","status":"publish","type":"page","link":"https:\/\/kmplg.sk\/?page_id=765","title":{"rendered":"RNDr. Ondrej Nemec, PhD."},"content":{"rendered":"\n
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poz\u00edcia<\/strong>:<\/td>odborn\u00fd asistent<\/td><\/tr>
miestnos\u0165<\/strong>:<\/td>G-328<\/td><\/tr>
telef\u00f3n<\/strong>:<\/td>+421 2 9014 9297<\/strong><\/td><\/tr>
e-mail:<\/strong><\/td>ondrej.nemec@uniba.sk<\/td><\/tr>
publik\u00e1cie<\/strong><\/td>zoznam publik\u00e1ci\u00ed<\/a><\/td><\/tr><\/tbody><\/table>
Oddelenie petrol\u00f3gie<\/span><\/figcaption><\/figure>\n<\/div>\n<\/div>\n\n\n\n

<\/p>\n<\/div><\/div>\n\n\n\n

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\"\" ResearchGate<\/span><\/a><\/div>\n\n\n\n
\"\"ORCID<\/span><\/a><\/div>\n\n\n\n
\"\" <\/span>Publons<\/span><\/a><\/div>\n\n\n\n
\"\" <\/span>Scopus<\/span><\/a><\/div>\n\n\n\n
T\u00e9my z\u00e1vere\u010dn\u00fdch pr\u00e1c<\/span><\/a><\/div>\n<\/div>\n<\/div>\n<\/div>\n\n\n\n

Vedeck\u00fd profil<\/h2>\n\n\n\n
  • petrol\u00f3gia, geoch\u00e9mia, mineral\u00f3gia a izotopov\u00e9 syst\u00e9my metab\u00e1zick\u00fdch a metapelitick\u00fdch horn\u00edn<\/li>
  • termodynamick\u00e9 modelovanie teplotno-tlakov\u00fdch (P-T-X<\/em>) podmienok<\/li>
  • vyu\u017e\u00edtie modern\u00fdch geotermobarometick\u00fdch met\u00f3dy a softv\u00e9rov\u00e9ho modelovania pomocou n\u00e1strojov ako TERMOCALC, Perple_X a MELTS<\/li>
  • v\u00fdskum \u0165a\u017ek\u00fdch miner\u00e1lov v bazaltoch Juhoslovensk\u00e9ho alkalicko-bazaltov\u00e9ho vulkanick\u00e9ho po\u013ea<\/li><\/ul>\n\n\n\n

    Pedagogick\u00e1 \u010dinnos\u0165<\/h2>\n\n\n\n

    Zameriava sa hlavne na v\u00fduku r\u00e1diog\u00e9nnych izotopov\u00fdch syst\u00e9mov, modern\u00fdch geotermobarometrick\u00fdch met\u00f3d a softv\u00e9rov\u00e9 modelovanie magmatick\u00fdch a metamorfn\u00fdch horninov\u00fdch syst\u00e9mov. <\/p>\n\n\n\n

    V\u00fduka v predmetoch na Bc. stupni<\/strong><\/p>\n\n\n\n

    • Petrografia metamorfovan\u00fdch horn\u00edn<\/li>
    • Petrografia magmatick\u00fdch horn\u00edn<\/li>
    • Mikroskopia horninotvorn\u00fdch miner\u00e1lov<\/li>
    • \u0164a\u017ek\u00e9 miner\u00e1ly<\/li>
    • Odrazov\u00e1 mikroskopia<\/li><\/ul>\n\n\n\n

      V\u00fduka v predmetoch na Mgr. stupni<\/strong><\/p>\n\n\n\n

      • Izotopov\u00e1 geol\u00f3gia<\/li>
      • Petrol\u00f3gia metamorfovan\u00fdch horn\u00edn<\/li>
      • Termodynamika a f\u00e1zov\u00e9 rovnov\u00e1hy<\/li>
      • Genetick\u00e1 mineral\u00f3gia horninov\u00fdch syst\u00e9mov<\/li><\/ul>\n\n\n\n

        V\u00fduka v predmetoch na PhD. stupni<\/strong><\/p>\n\n\n\n

        • Izotopov\u00e1 geol\u00f3gia a geochronol\u00f3gia<\/li><\/ul>\n\n\n\n
          \n\n\n\n

          Vybran\u00e9 najv\u00fdznamnej\u0161ie publik\u00e1cie<\/h2>\n\n\n\n
          \n
          • Nemec, O.,Puti\u0161, M., Ba\u010d\u00edk, P., Ru\u017ei\u010dka, P., N\u00e9meth, Z., 2020: Metamorphic Conditions of Neotethyan Meliatic Accretionary Wedge Estimated by Thermodynamic Modelling and Geothermobarometry (Inner Western Carpathians)<\/strong>. Minerals<\/em>, 10, 1-50, 1094.<\/li>
          • Puti\u0161 M., Sot\u00e1k J., Li Q.-L., Ondrejka M., Li X.-H., Hu Z., Ling X., Nemec O., N\u00e9meth Z., Ru\u017ei\u010dka P. 2019: Origin and Age Determination of the Neotethys Meliata Basin Ophiolite Fragments in the Late Jurassic\u2013Early Cretaceous Accretionary Wedge M\u00e9lange (Inner Western Carpathians, Slovakia)<\/strong>. Minerals<\/em>, 9, 652.<\/li>
          • Paquette J-L., Huraiov\u00e1 M., Nemec O., Gannoun A., \u0160arinov\u00e1 K, Hurai V. 2019: Origin and provenance of 2 Ma\u20132 Ga zircons ejected by phreatomagmatic eruptions of Pliocene basalts in southern Slovakia<\/strong>. International Journal of Earth Sciences<\/em>, 108 (8), 2607\u20132623.<\/li>
          • Nemec O., Huraiov\u00e1 M. 2018: Provenance study of detrital garnets and rutiles from basaltic pyroclastic rocks of Southern Slovakia (Western Carpathians)<\/strong>, Geologica Carpathica<\/em>, 69 (1), 17\u201329.<\/li><\/ul>\n<\/div><\/div>\n\n\n\n

            Aktu\u00e1lne rie\u0161en\u00e9 projekty<\/h2>\n\n\n\n

            APVV-19-0065 \u2013 \u010dlen rie\u0161ite\u013esk\u00e9ho kolekt\u00edvu<\/strong><\/strong> (2020-2023, hlavn\u00fd rie\u0161ite\u013e M. Puti\u0161) \u201ePetrologicko-geochronologick\u00fd z\u00e1znam riftogen\u00e9zy a k\u00f4rovo- pl\u00e1\u0161\u0165ovej recykl\u00e1cie v orog\u00e9nnej prizme Z\u00e1padn\u00fdch Karp\u00e1t\u201d Klikni pre podrobnosti o projekte<\/span>

            Predmetom v\u00fdskumu s\u00fa \u0161pecifick\u00e9 skupiny k\u00f4rov\u00fdch a pl\u00e1\u0161\u0165ov\u00fdch horn\u00edn a ich miner\u00e1lov ako indik\u00e1torov riftog\u00e9nnych z\u00f3n a to aj napriek tomu, \u017ee \u010dasto maj\u00fa znaky mlad\u0161ieho tektono-term\u00e1lneho prepracovania v d\u00f4sledku ich za\u010dlenenia do orogenetick\u00fdch z\u00f3n. Pou\u017e\u00edvame mineralogicko-petrologick\u00e9 (EPMA, micro-Raman, LA-ICP-MS, XRF, ICP-MS), izotopovo-geochemick\u00e9 (LA-MC-ICP-MS, TIMS) a geochronologick\u00e9 (U-Pb SIMS, LA-ICP-MS, Ar-Ar, K-Ar) met\u00f3dy na ur\u010denie chemizmu miner\u00e1lov a horn\u00edn, vr\u00e1tane vybran\u00fdch r\u00e1diog\u00e9nnych izotopov (U-Pb, Pb-Pb, Sm-Nd, Rb-Sr, Zr-Hf, Re-Os) na ur\u010denie ich veku a gen\u00e9zy.<\/em><\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

            VEGA 1\/0143\/18 \u2013 \u010dlen rie\u0161ite\u013esk\u00e9ho kolekt\u00edvu<\/strong><\/strong> (2018-2021, hlavn\u00fd rie\u0161ite\u013e M. Huraiov\u00e1) \u201eMineral\u00f3gia, petrogen\u00e9za a metalogenetick\u00fd potenci\u00e1l vn\u00fatro-plat\u0148ov\u00e9ho magmatizmu Z\u00e1padn\u00fdch Karp\u00e1t\u201d Klikni pre podrobnosti o projekte<\/span>

            Alkalick\u00e9 bazalty na ju\u017enom Slovensku obsahuj\u00fa xenolity magmatick\u00fdch horn\u00edn, ktor\u00e9 sa nevyskytuj\u00fa inde v Z\u00e1padn\u00fdch Karpatoch. Pozorovan\u00e9 typy horn\u00edn zah\u0155\u0148aj\u00fa mafick\u00e9 gabroidn\u00e9 kumul\u00e1ty, syenity, granity, karbonatity, ako aj metasomatick\u00e9 produkty interakcie magmy s k\u00f4rou (skarny). Magmatick\u00e9 horniny vznikli pri frak\u010dnej kry\u0161taliz\u00e1cii bazaltovej magmy a parci\u00e1lnom taven\u00ed k\u00f4ry. Cie\u013eom projektu je mineralogick\u00e1, geochemick\u00e1, geochronologick\u00e1 a petrologick\u00e1 charakteristika magmatick\u00fdch horn\u00edn, zhodnotenie ich gen\u00e9zy, geotektonick\u00e9ho prostredia, zdroja a metalogenetick\u00e9ho potenci\u00e1lu s oh\u013eadom na mo\u017en\u00fd v\u00fdskyt kritick\u00fdch prvkov (Nb, Ta, U, Th, vz\u00e1cne zeminy). \u010eal\u0161\u00edm cie\u013eom projektu je rekon\u0161trukcia zlo\u017eenia predterci\u00e9rnej k\u00f4ry v oblasti ju\u017en\u00e9ho Slovenska<\/em><\/em>. <\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

            VEGA 1\/0151\/19<\/strong> \u2013 \u010dlen rie\u0161ite\u013esk\u00e9ho kolekt\u00edvu<\/strong><\/strong> (2019-2021, hlavn\u00fd rie\u0161ite\u013e prof. M. Puti\u0161) \u201ePetrochnonol\u00f3gia pl\u00e1\u0161\u0165ov\u00fdch a k\u00f4rov\u00fdch dajkov\u00fdch syst\u00e9mov v kriedovej akre\u010dnej prizme Z\u00e1padn\u00fdch Karp\u00e1t a v\u00fdchodnom okraji austroalpinika\u201d Klikni pre podrobnosti o projekte<\/span>

            <\/span>Kriedov\u00e1 akre\u010dn\u00e1 prizma orog\u00e9nu Vn\u00fatorn\u00fdch Z\u00e1padn\u00fdch Karp\u00e1t a austroalpinika \u00c1lp obsahuje dajky k\u00f4rov\u00fdch a pl\u00e1\u0161\u0165ov\u00fdch horn\u00edn. Ich magmatick\u00fd v\u00fdvoj je indik\u00e1torom permsko-triasovej, alebo jursko-kriedovej extenzie a otv\u00e1rania oce\u00e1nov neotet\u00fddy a atlantickej tet\u00fddy. Ich metamorf\u00f3za odr\u00e1\u017ea paleotektonick\u00e9 prostredie, ale aj geodynamick\u00fd v\u00fdvoj Karp\u00e1t a \u00c1lp po uzavret\u00ed t\u00fdchto oce\u00e1nov. Miner\u00e1lne zlo\u017eenie (EMPA, LA-ICP-MS) a celohorninov\u00fd chemizmus (ICP-MS) bud\u00fa vyu\u017eit\u00e9 na defin\u00edciu ich magmatick\u00e9ho p\u00f4vodu p\u00f4vodu. Izotopick\u00e9 zlo\u017eenie (Rb\/Sr, Lu\/Hf, Sm\/Nd, U\/Pb) poskytne inform\u00e1ciu o ich pl\u00e1\u0161\u0165ovom \u010di k\u00f4rovom zdroji. Izotopick\u00e9 datovanie (U-Pb SIMS, nano-SIMS, LA-MC-ICP-MS, K-Ar) umo\u017en\u00ed vytvorenie geodynamick\u00e9ho modelu v\u00fdvoja dajkov\u00fdch syst\u00e9mov v akre\u010dn\u00fdch komplexoch. P-T podmienky magmatickej a metamorfnej etapy bud\u00fa modelovan\u00e9 najnov\u0161\u00edmi termodynamick\u00fdmi softv\u00e9rmi (Melts, Perple_X, Thermocalc). Pos\u00fadi sa ich ekonomick\u00fd potenci\u00e1l. <\/span><\/em><\/em><\/p>\n\n\n\n

            <\/div><\/span><\/p>\n","protected":false},"excerpt":{"rendered":"

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