{"id":740,"date":"2021-03-31T08:12:36","date_gmt":"2021-03-31T06:12:36","guid":{"rendered":"http:\/\/d.r1.wbsprt.com\/kmplg.sk\/?page_id=740"},"modified":"2023-01-30T09:20:49","modified_gmt":"2023-01-30T08:20:49","slug":"rndr-jana-fridrichova-phd","status":"publish","type":"page","link":"https:\/\/kmplg.sk\/?page_id=740","title":{"rendered":"Doc. RNDr. Jana Fridrichov\u00e1, PhD."},"content":{"rendered":"\n
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poz\u00edcia<\/strong><\/td>docentka<\/td><\/tr>
miestnos\u0165<\/strong> <\/td>G-348<\/td><\/tr>
tel: <\/strong><\/td>+421 2 9014 9294<\/strong><\/td><\/tr>
e-mail:<\/strong> <\/td>jana.fridrichova@uniba.sk<\/td><\/tr>
publik\u00e1cie<\/strong><\/td>zoznam publik\u00e1ci\u00ed<\/a><\/td><\/tr><\/tbody><\/table>
Oddelenie mineral\u00f3gie a kry\u0161talografie<\/span><\/figcaption><\/figure>\n<\/div>\n<\/div>\n<\/div><\/div>\n\n\n\n
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\"\"ResearchGate<\/a><\/div>\n\n\n\n
\"\"Scopus<\/a><\/div>\n\n\n\n
\"\"ORCID<\/a><\/div>\n<\/div>\n\n\n\n

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

Vedeck\u00fd profil<\/h2>\n\n\n\n
  • silik\u00e1tov\u00e1 mineral\u00f3gia<\/li>
  • kry\u0161taloch\u00e9mia<\/li>
  • gemol\u00f3gia<\/li>
  • spektroskopick\u00e9 analytick\u00e9 met\u00f3dy<\/li>
  • experiment\u00e1lna mineral\u00f3gia a gemol\u00f3gia<\/li><\/ul>\n\n\n\n

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

    Zameriava sa hlavne na v\u00fduku mineral\u00f3gie, gemol\u00f3gie, kry\u0161talografie, kry\u0161taloch\u00e9mie a analytick\u00fdch met\u00f3d v mineral\u00f3gii.<\/p>\n\n\n\n

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

    • Mineral\u00f3gia 1<\/li>
    • Morfologick\u00e1 a \u0161trukt\u00farna kry\u0161talografia <\/li>
    • Z\u00e1klady gemol\u00f3gie<\/li><\/ul>\n\n\n\n

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

      • Kry\u0161taloch\u00e9mia silik\u00e1tov <\/li>
      • Systematick\u00e1 gemol\u00f3gia<\/li>
      • Rtg. difraktometria <\/li>
      • Kry\u0161talochemick\u00e9 prepo\u010dty<\/li>
      • Laborat\u00f3rne met\u00f3dy v mineral\u00f3gii a petrol\u00f3gii <\/li>
      • Kry\u0161talochemick\u00fd semin\u00e1r <\/li>
      • Mineral\u00f3gia prachov\u00fdch \u010dast\u00edc v atmosf\u00e9re<\/li><\/ul>\n\n\n\n

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

        • Kry\u0161taloch\u00e9mia silik\u00e1tov\u00fdch miner\u00e1lov<\/li>
        • Kry\u0161taloch\u00e9mia nesilik\u00e1tov\u00fdch miner\u00e1lov<\/li>
        • Mineral\u00f3gia horn\u00edn<\/li>
        • Laborat\u00f3rne met\u00f3dy v\u00fdskumu miner\u00e1lov<\/li>
        • Mineral\u00f3gia \u017eivotn\u00e9ho prostredia<\/li><\/ul>\n\n\n\n
          \n\n\n\n

          Vybran\u00e9 najv\u00fdznamnej\u0161ie publik\u00e1cie<\/h2>\n\n\n\n
          \n
          • Ba\u010d\u00edk P., Miyawaki R., Atencio D., C\u00e1mara F., Fridrichov\u00e1 J.<\/strong>, 2017: Nomenclature of gadolinite supergroup<\/strong>. European Journal of Mineralogy, 29, 1067-1082<\/li>
          • Fridrichov\u00e1 J.<\/strong>, Ba\u010d\u00edk P., Ertl A., Wildner M., Miglierini M., 2018: Crystal chemistry and Jahn-Teller distortion of Mn3+-occupied octahedra in red beryl from Utah<\/strong>. Journal of Molecular Structure, 1152, 79-86<\/li>
          • Fridrichov\u00e1 J.<\/strong>, Ba\u010d\u00edk P., Ill\u00e1\u0161ov\u00e1 \u013d., Koz\u00e1kov\u00e1 P., \u0160koda R., Puli\u0161ov\u00e1 Z., Fiala A., 2016: Raman and optical spectroscopic investigation of gem-quality smoky quartz<\/strong>. Vibrational Spectroscopy, 85, 71-78<\/li>
          • Fridrichov\u00e1 J.<\/strong>, Ba\u010d\u00edk P., Bizovsk\u00e1 V., Libowitzky E., \u0160koda R., Uher P., Ozd\u00edn D., \u0160tevko M., 2016: Spectroscopic and bond-topological investigation of interstitial volatiles in beryl from Slovakia<\/strong>. Physics and Chemistry Minerals, 43, 419-437<\/li>
          • Fridrichov\u00e1 J.<\/strong>, Ba\u010d\u00edk P., Rusinov\u00e1 P., Antal P., \u0160koda R., Bizovsk\u00e1 V., Miglierini M., 2015: Optical and crystal-chemical changes in aquamarines and yellow beryls from Thanh Hoa province, Vietnam induced by heat treatment<\/strong>. Physics and Chemistry Minerals, 42, 287-302.<\/li><\/ul>\n<\/div><\/div>\n\n\n\n

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

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

            APVV-18-0065 – rie\u0161ite\u013eka<\/strong> (2018-2023, hlavn\u00fd rie\u0161ite\u013e doc. P. Ba\u010d\u00edk) \u201e\u013dahk\u00e9 litofiln\u00e9 prvky (Li, Be, B) vo vybran\u00fdch miner\u00e1loch: od kry\u0161t\u00e1lovej \u0161trukt\u00fary ku geologick\u00fdm procesom \/ Light litophile elements (Li, Be, B) in selected minerals: from crystal structure to geological processes\u201d (Klikni pre podrobnosti o projekte<\/em>)<\/span>

            V r\u00e1mci projektu s\u00fa sk\u00faman\u00e9 mineralogick\u00e9 a kry\u0161talochemick\u00e9 \u0161t\u00fadium miner\u00e1lov, ktor\u00e9 obsahuj\u00fa vo svojej \u0161trukt\u00fare \u013eahk\u00e9 kati\u00f3ny druhej peri\u00f3dy periodickej s\u00fastavy \u2013 l\u00edtium, ber\u00fdlium a b\u00f3r. V\u00fdskum sa teda orientuje na dve oblasti a bud\u00fa sk\u00faman\u00e9 dva typy miner\u00e1lov. Prv\u00e1 oblas\u0165 v\u00fdskumu sa s\u00fastre\u010fuje na kry\u0161talochemick\u00e9 z\u00e1konitosti a\u017e na subatom\u00e1rnej \u00farovni pomocou najmodernej\u0161\u00edch analytick\u00fdch met\u00f3d. Druh\u00e1 oblas\u0165 bude orientovan\u00e1 na spr\u00e1vanie t\u00fdchto prvkov v miner\u00e1lnom a horninovom prostred\u00ed. Z miner\u00e1lov s\u00fa \u0161tudovan\u00e9 tie, ktor\u00e9 obsahuj\u00fa Be, B a Li ako prvky obsiahnut\u00e9 priamo v ich kry\u0161talochemickom vzorci, teda tieto prvky s\u00fa dominantn\u00e9 minim\u00e1lne v jednej \u0161trukt\u00farnej poz\u00edcii. Patria sem najm\u00e4 silik\u00e1ty (turmal\u00ednov\u00e1 superskupina, gadolinitov\u00e1 superskupina, berylov\u00e1 a kordieritov\u00e1 skupina, Li s\u013eudy, spodumen, bertrandit, fenakit), bor\u00e1ty (cel\u00e1 trieda), fosf\u00e1ty (herderitov\u00e1 skupina) a oxidy (chryzoberyl). Sk\u00faman\u00e9 v\u0161ak bud\u00fa aj miner\u00e1ly, v ktor\u00fdch Be, B a Li substituuj\u00fa ostatn\u00e9 kati\u00f3ny, ale nie s\u00fa dominantn\u00e9, s\u00fa minoritn\u00e9 a\u017e stopov\u00e9. V r\u00e1mci toho sa bude \u0161tudova\u0165 distrib\u00facia \u0161tudovan\u00fdch prvkov v r\u00f4znych miner\u00e1loch vo variabiln\u00fdch horninov\u00fdch prostrediach. \/ The project includes mineralogical and crystal-chemical studies of minerals that contain light cations from the second period of the periodic system – lithium, beryllium and boron in their structure. Research is focused on two areas and two types of minerals will be examined. The first area of research will focus on crystal-chemical patterns down to the subatomic level using state-of-the-art analytical methods. The second area will be focused on the behaviour of these elements in the mineral and rock environment. Firstly, minerals containing Be, B and Li directly in their crystal-chemical formula (these elements are dominant at least at one structural site) will be studied. These include silicates (tourmaline supergroup, gadolinite supergroup, beryl and cordierite, Li mica, spodumen, bertrandite, phenakite), borates (whole class), phosphates (herderite) and oxides (chrysoberyl). However, we will focus also on the minerals in which Be, B and Li substitute for the other cations, but are not dominant. In this context, the distribution of studied elements in various minerals in variable rock environments will be studied.<\/em><\/span><\/p>\n\n\n\n

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

            VEGA 1\/0137\/20 – rie\u0161ite\u013eka<\/strong> (2020-2022, hlavn\u00fd rie\u0161ite\u013e doc. P. Ba\u010d\u00edk) \u201eExperiment\u00e1lne \u0161t\u00fadium fyzik\u00e1lno-chemick\u00fdch vlastnost\u00ed vybran\u00fdch miner\u00e1lov (oxidov, fosf\u00e1tov a silik\u00e1tov)\/Experimental study of physico-chemical properties of selected minerals (oxides, phosphates and silicates).\u201d (Klikni pre podrobnosti o projekte)<\/em><\/span>

            Experiment\u00e1lny v\u00fdskum miner\u00e1lov je vhodn\u00fd na detailn\u00e9 kry\u0161talochemick\u00e9 \u0161t\u00fadium vlastnost\u00ed a procesov v r\u00e1mci \u0161trukt\u00fary a jej stability, ale aj na \u00fapravu vlastnost\u00ed drah\u00fdch kame\u0148ov v r\u00e1mci gemol\u00f3gie. Niektor\u00e9 z t\u00fdchto experimentov nie s\u00fa dostato\u010dne op\u00edsan\u00e9 a nie je zn\u00e1my mechanizmus sp\u00f4sobuj\u00faci zmenu farby, ani procesy ved\u00face k rozpadu \u0161trukt\u00fary miner\u00e1lov. Pomocou tepeln\u00fdch, tepelno-tlakov\u00fdch a radia\u010dn\u00fdch experimentov bud\u00fa \u0161tudovan\u00e9 kry\u0161talochemick\u00e9 procesy vo vybran\u00fdch miner\u00e1loch (oxidoch, fosf\u00e1toch a silik\u00e1toch), pri\u010dom ide najm\u00e4 o oxid\u00e1ciu alebo redukciu kati\u00f3nov, vznik alebo z\u00e1nik farebn\u00fdch centier a \u0161trukt\u00farnych defektov. Pri experiment\u00e1lnych podmienkach bud\u00fa \u0161tudovan\u00e9 aj procesy rozpadu \u0161trukt\u00fary miner\u00e1lov a produkty vzniku nov\u00fdch f\u00e1z.\/ The experimental mineralogical approach is suitable for detailed crystal-chemical study of properties and processes within the crystal structure and its stability, but also for the precious stones treatment within the gemmology. Some of these experiments are not sufficiently described and the colour changing mechanisms are similarly not clearly known as well as the processes leading to the mineral structure breakdown. The crystal-chemical properties of selected minerals (oxides, phosphates and silicates) will be studied by thermal, thermal-pressure and radiation experiments, especially the oxidation or reduction of cations, the formation or disappearance of colour centres and structural defects. The mineral decomposition processes and new phase formation will also be studied under experimental conditions.<\/em><\/em><\/span> <\/p>\n\n\n\n<\/div>\n\n\n\n

            VEGA-1\/0151\/19<\/strong> – rie\u0161ite\u013eka<\/strong> (2019-2021, hlavn\u00fd rie\u0161ite\u013e prof. M. Puti\u0161) \u201ePetrol\u00f3gia a geochronol\u00f3gia k\u00f4rov\u00fdch a pl\u00e1\u0161\u0165ov\u00fdch dajkov\u00fdch syst\u00e9mov v kriedovej akre\u010dnej prizme Z\u00e1padn\u00fdch Karp\u00e1t a v\u00fdchodn\u00e9ho okraja austroalpinik\/Petrology and geochronology of crustal and mantle dyke systems in Cretaceous accretionary wedge of the Western Carpathians and eastern Austroalpine margin\u201d (Klikni pre podrobnosti o projekte)<\/em><\/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. Vyu\u017eijeme mo\u017enosti medzin\u00e1rodnej spolupr\u00e1ce pre izotopov\u00fa geochronol\u00f3giu. \/ Cretaceous accretionary wedges of the Western Carpathians and the Austro-Alpine unit of the eastern Alps contains dykes of the crustal and mantle rocks. These rocks are significant indicator of Permian-Triassic or Jurassic-Cretaceous extension and the opening of the Neotethys and Atlantic Tethys respectively. They are of the key importance for the reconstruction of palaeotectonic and geodynamic evolution of the Carpathians and Alps. The mineral rock composition (EPMA, LA-ICP-MS) and their whole-rock chemistry (ICP-MS) will be used for definition of their palaeotectonic origin. The isotopic study (Rb\/Sr, Lu\/Hf, Sm\/Nd. U\/Pb) of the rocks and minerals, and their isotopic dating (U-Pb SIMS, nano-SIMS, LA-MC-ICP-MS, K-Ar) will enhance creation of geodynamic evolution model of mentioned accretionary complexes. Their occasional economic potential can be estimated. We will utilize possibilities of our broad international co-operation particularly in isotope geochronology.<\/em><\/em><\/span><\/p>\n\n\n\n

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

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