{"id":85,"date":"2021-03-05T06:34:48","date_gmt":"2021-03-05T05:34:48","guid":{"rendered":"http:\/\/d.r1.wbsprt.com\/kmplg.sk\/?page_id=85"},"modified":"2025-02-24T09:56:43","modified_gmt":"2025-02-24T08:56:43","slug":"temy-zaverecnych-prac","status":"publish","type":"page","link":"https:\/\/kmplg.sk\/?page_id=85","title":{"rendered":"T\u00e9my z\u00e1vere\u010dn\u00fdch pr\u00e1c"},"content":{"rendered":"\n
\n
Bakal\u00e1rske pr\u00e1ce<\/span><\/a><\/div>\n\n\n\n
Diplomov\u00e9 pr\u00e1ce<\/a><\/div>\n\n\n\n
Dizerta\u010dn\u00e9 pr\u00e1ce<\/a><\/div>\n<\/div>\n\n\n\n

Zvo\u013e typ z\u00e1vere\u010dnej pr\u00e1ce<\/em><\/p>\n\n\n\n

\n\n\n\n

Bakal\u00e1rske pr\u00e1ce<\/span><\/h2>\n\n\n\n

2019\/2020<\/span><\/strong><\/h4>\n\n\n\n

Mineralogick\u00e1 a genetick\u00e1 charakteristika mineraliz\u00e1ci\u00ed v pohor\u00ed Tribe\u010d<\/strong> – \u0161kolite\u013e Daniel Ozd\u00edn Klikni pre viac inform\u00e1ci\u00ed<\/span>

Cie\u013eom pr\u00e1ce je zosumarizova\u0165 poznatky o v\u0161etk\u00fdch typoch najm\u00e4 hydroterm\u00e1lnych mineraliz\u00e1ci\u00ed v pohor\u00ed Tribe\u010d – mineralogick\u00e1 charakteristika a genetick\u00e9 podmienky vzniku. Pr\u00e1ca je zameran\u00e1 najm\u00e4 na alpinotypn\u00e9 mineraliz\u00e1cie.<\/em><\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Metodick\u00e9 postupy a procesy mechanickej \u00fapravy, \u010distenia, stabiliz\u00e1cie a konzerv\u00e1cie miner\u00e1lov pri mineralogickom v\u00fdskume a depoz\u00edcii v muze\u00e1lnych zbierkach<\/strong> – \u0161kolite\u013e Daniel Ozd\u00edn Klikni pre viac inform\u00e1ci\u00ed<\/span>

Cie\u013eom pr\u00e1ce je komplexn\u00e9 kry\u0161talochemick\u00e9 \u0161t\u00fadium experiment\u00e1lnych \u00faprav berylu. \u0160tudovan\u00e9 bud\u00fa preva\u017ene drahokamov\u00e9 berylov\u00e9 variety – akvamar\u00edn, heliodor, morganit. Experiment\u00e1lne \u00fapravy zah\u0155\u0148aj\u00fa zahrievanie na teploty na stovky stup\u0148ov Celzia a o\u017earovanie. Praktick\u00fdm v\u00fdstupom je odha\u013eovanie \u00faprav drahokamov\u00fdch variet berylu v r\u00e1mci forenznej gemol\u00f3gie.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Kry\u0161talochemick\u00e9 \u0161t\u00fadium experiment\u00e1lnych \u00faprav berylu<\/strong> – \u0161kolite\u013e Jana Fridrichov\u00e1 Klikni pre viac inform\u00e1ci\u00ed<\/span>

Cie\u013eom pr\u00e1ce je zhrn\u00fa\u0165 doteraj\u0161ie poznatky z analytick\u00fdch met\u00f3d, procesov \u010distenia, mechanickej \u00fapravy vzoriek a konzerv\u00e1cie miner\u00e1lov a charakteristika metodick\u00fdch postupov pou\u017e\u00edvan\u00fdch pri mineralogickom v\u00fdskume a fin\u00e1lnej \u00faprave vzoriek na v\u00fdskumn\u00e9, expozi\u010dn\u00e9 a depozi\u010dn\u00e9 \u00fa\u010dely.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

2020\/2021<\/span><\/strong><\/h4>\n\n\n\n

Karbonatity – mineral\u00f3gia, petrol\u00f3gia a lo\u017eisk\u00e1<\/strong> – \u0161kolite\u013e Monika Huraiov\u00e1 Klikni pre viac inform\u00e1ci\u00ed<\/span>

Karbonatit – exotick\u00e1 magmatick\u00e1 hornina, jej miner\u00e1lne zlo\u017eenie, petrol\u00f3gia, v\u00fdskyt a lo\u017eisk\u00e1.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Lo\u017eisk\u00e1 volfr\u00e1mu vo svete a na Slovensku a ich gen\u00e9za<\/strong> – \u0161kolite\u013e Peter Kod\u011bra Klikni pre viac inform\u00e1ci\u00ed<\/span>

<\/span> Zhrnutie vlastnosti, zdrojov a s\u00fa\u010dasn\u00fdch perspekt\u00edv vyu\u017eitia kritickej suroviny kobaltu, genetick\u00e9 typy lo\u017e\u00edsk kobaltu a ich distrib\u00facia vo svete. Pr\u00edklady v\u00fdznamn\u00fdch svetov\u00fdch a slovensk\u00fdch lo\u017e\u00edsk kobaltu a ich postavenie v metalogen\u00e9ze Slovenska. Praktick\u00fd v\u00fdskum paleofluid na lo\u017eisku Hn\u00fa\u0161\u0165a-M\u00fatnik<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Lo\u017eisk\u00e1 kobaltu vo svete a na Slovensku a ich gen\u00e9za<\/strong> – \u0161kolite\u013e Peter Kod\u011bra Klikni pre viac inform\u00e1ci\u00ed<\/span>

Zhrnutie vlastnosti, zdrojov a s\u00fa\u010dasn\u00fdch perspekt\u00edv vyu\u017eitia kritickej suroviny kobaltu, genetick\u00e9 typy lo\u017e\u00edsk kobaltu a ich distrib\u00facia vo svete. Pr\u00edklady v\u00fdznamn\u00fdch svetov\u00fdch a slovensk\u00fdch lo\u017e\u00edsk kobaltu a ich postavenie v metalogen\u00e9ze Slovenska. Praktick\u00fd v\u00fdskum paleofluid na lo\u017eisku Hn\u00fa\u0161\u0165a-M\u00fatnik<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

2021\/2022<\/span><\/strong><\/h4>\n\n\n\n

Vz\u00e1cne litofiln\u00e9 prvky (Li, Be, B, REE, Zr-Hf, Nb-Ta) v biominer\u00e1loch<\/strong> – \u0161kolite\u013e Pavel Uher Klikni pre viac inform\u00e1ci\u00ed<\/span>

Zhrnutie s\u00fa\u010dasn\u00fdch poznatkov o distrib\u00facii vz\u00e1cnych litofiln\u00fdch prvkov v r\u00f4znych typoch fos\u00edlnych aj recentn\u00fdch biominer\u00e1lov, ich miner\u00e1lne formy a mechanizmus vzniku<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

\u013dahk\u00e9 litofiln\u00e9 prvky (Li, Be, B) vo vybran\u00fdch horninotvorn\u00fdch a akcesorick\u00fdch miner\u00e1loch<\/strong> – \u0161kolite\u013e Pavel Uher Klikni pre viac inform\u00e1ci\u00ed<\/span>

Zhrnutie s\u00fa\u010dasn\u00fdch poznatkov o distrib\u00facii vz\u00e1cnych litofiln\u00fdch prvkov (Li, Be, B) v niketor\u00fdch petrogeneticky d\u00f4le\u017eit\u00fdch miner\u00e1lov (kreme\u0148, \u017eivce, gran\u00e1ty, spinelidy, skupina epidotu a vesuvianitu)<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Relikty oce\u00e1nskej k\u00f4ry paleozoika a mezozoika Z\u00e1padn\u00fdch Karp\u00e1t: geol\u00f3gia a petrografia<\/strong> – \u0161kolite\u013e Mari\u00e1n Puti\u0161 Klikni pre viac inform\u00e1ci\u00ed<\/span>

Geologick\u00fd preh\u013ead v\u00fdskytov reliktov oce\u00e1nskej k\u00f4ry; petrografick\u00fd opis meta-ofiolitov; zostava litologick\u00fdch profilov z literat\u00fary; z\u00e1kladn\u00e9 petrologicko-geochemick\u00e9 charakteristiky; preh\u013ead vekov (geochronol\u00f3gia). V\u00fdber ofiolitick\u00e9ho komplexu na pokra\u010dovanie v diplomovej pr\u00e1ci.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Kontamin\u00e1cia rie\u010dnych sedimentov v oblastiach ovplyvnen\u00fdch \u0165a\u017ebou nerastn\u00fdch surov\u00edn.<\/strong> – \u0161kolite\u013e Peter \u0160ottn\u00edk Klikni pre viac inform\u00e1ci\u00ed<\/span>

Cie\u013eom pr\u00e1ce bude z\u00edskanie poznatkov o: v\u0161eobecnom miner\u00e1lnom zlo\u017een\u00ed rie\u010dnych sedimentov, \u0161pecifik\u00e1ch kontamin\u00e1cie rie\u010dnych sedimentov v oblastiach ovplyvnen\u00fdch \u0165a\u017ebou nerastn\u00fdch surov\u00edn, form\u00e1ch vystupovania jednotliv\u00fdch kontaminuj\u00facich l\u00e1tok v rie\u010dnych sedimentoch<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Porovnanie mobility As a Sb v pr\u00edrodnom prostred\u00ed<\/strong> – \u0161kolite\u013e Peter \u0160ottn\u00edk Klikni pre viac inform\u00e1ci\u00ed<\/span>

<\/span> Mobilita arz\u00e9nu a anti\u00f3nu v jednotliv\u00fdch zlo\u017ek\u00e1ch \u017eivotn\u00e9ho prostredia. Definovanie rozdielov v spr\u00e1van\u00ed As a Sb v \u017eivotnom prostred\u00ed.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

\u00cdly na biomedic\u00ednske, lie\u010debn\u00e9 a farmaceutick\u00e9 pou\u017eitie<\/strong> – \u0161kolite\u013e Peter Uhl\u00edk Klikni pre viac inform\u00e1ci\u00ed<\/span>

<\/span> Zvl\u00e1dnu\u0165 z\u00e1kladn\u00fa charakteristiku \u0161trukt\u00fary vrstevnat\u00fdch silik\u00e1tov a ich vlastnost\u00ed. Vy\u010dleni\u0165 oblasti kde \u00edlov\u00e9 miner\u00e1ly p\u00f4sobia pozit\u00edvne pri lie\u010dbe a pok\u00fasi\u0165 sa \u0161pecifikova\u0165 ich v\u00fdznam. Zadefinova\u0165 ich funkciu pri peror\u00e1lnej a derm\u00e1lnej aplik\u00e1cii.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Mo\u017enosti vyu\u017eitia TEM v geoved\u00e1ch<\/strong> – \u0161kolite\u013e Peter Uhl\u00edk Klikni pre viac inform\u00e1ci\u00ed<\/span>

Stru\u010dn\u00e1 charakteristika z\u00e1kladn\u00fdch princ\u00edpov transmisnej elektr\u00f3novej mikroskopie. Preh\u013ead metod\u00edk pr\u00edpravy vzoriek, ich mo\u017enosti pozorovania TEM a mo\u017en\u00e9 v\u00fdstupy Perspekt\u00edvne oblasti vyu\u017eitia TEM (vybra\u0165 zauj\u00edmav\u00e9 pr\u00edklady aplik\u00e1cie TEM v pedol\u00f3gii, environmentalistike, mineral\u00f3gii, v oblasti spracovania nerastn\u00fdch surov\u00edn at\u010f.; pr\u00edpadne navrhn\u00fa\u0165 vlastn\u00e9 n\u00e1pady)<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Bentonit<\/strong> – \u0161kolite\u013e Peter Uhl\u00edk Klikni pre viac inform\u00e1ci\u00ed<\/span>

Charakterizova\u0165 smektit ako hlavn\u00fd miner\u00e1l bentonitov. Charakterizova\u0165 vznik lo\u017e\u00edsk bentonitu. Zozbiera\u0165 poznatky o \u0165a\u017ebe bentonitu doma i v zahrani\u010d\u00ed. Uvies\u0165 u\u017eitkov\u00e9 vlastnosti a vyu\u017eitie pr\u00edrodn\u00e9ho a upraven\u00e9ho bentonitu. \u010co ovplyv\u0148uje cenu bentonitu?<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Geol\u00f3gia a enol\u00f3gia<\/strong> – \u0161kolite\u013e Peter Uhl\u00edk Klikni pre viac inform\u00e1ci\u00ed<\/span>

Vymenova\u0165 faktory ovplyv\u0148uj\u00face kvalitu vini\u010da hroznorod\u00e9ho. \u00daloha geol\u00f3gie vo vin\u00e1rstve. Definova\u0165 terroir a faktory, ktor\u00e9 ho ovplyv\u0148uj\u00fa. Charakterizova\u0165 vplyv horninov\u00e9ho substr\u00e1tu na kvalitu vini\u010da hroznorod\u00e9ho. \u00daloha geoch\u00e9mie pri ur\u010dovan\u00ed p\u00f4vodu v\u00edna<\/span>.<\/p>\n\n\n\n<\/div>\n\n\n\n

Aplik\u00e1cia 3D modelovania vo v\u00fdskume lo\u017e\u00edsk nerastn\u00fdch surov\u00edn<\/strong> – \u0161kolite\u013e Jana Br\u010dekov\u00e1 Klikni pre viac inform\u00e1ci\u00ed<\/span>

Zhrn\u00fa\u0165 s\u00fa\u010dasn\u00e9 trendy v problematike 3D modelovania lo\u017e\u00edsk nerastn\u00fdch surov\u00edn, v\u00fdhody a nev\u00fdhody pou\u017e\u00edvan\u00fdch metodick\u00fdch postupov. Charakterizova\u0165 vstupn\u00e9 \u00fadaje z lo\u017eiskov\u00e9ho prieskumu a sp\u00f4sob ich spracovania. Charakterizova\u0165 \u00fadaje z vedeck\u00e9ho v\u00fdskumu a hlavn\u00e9 met\u00f3dy mineralogick\u00e9ho a geochemick\u00e9ho v\u00fdskumu zohr\u00e1vaj\u00face \u00falohu pri modelovan\u00ed parametrov vn\u00fatornej stavby lo\u017e\u00edsk. Zhrnutie ak\u00fdm sp\u00f4sobom s\u00fa \u00fadaje v\u010dlenen\u00e9 do 3D modelovania. Charakterizovanie postupov pri zhotovovan\u00ed lo\u017eiskovo-geologick\u00fdch a geochemnick\u00fdch modelov lo\u017e\u00edsk nerastn\u00fdch surov\u00edn s oh\u013eadom na typ lo\u017e\u00edsk nerastn\u00fdch surov\u00edn.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n
\n\n\n\n

Diplomov\u00e9 pr\u00e1ce<\/span><\/h2>\n\n\n\n

2020\/2021<\/span><\/strong><\/h4>\n\n\n\n

Kry\u0161talochemick\u00e9 a spektroskopick\u00e9 \u0161t\u00fadium farebn\u00fdch variet turmal\u00ednov<\/strong> – \u0161kolite\u013e Ba\u010d\u00edk Peter<\/p>\n\n\n\n

3D modelovanie vybran\u00fdch parametrov lo\u017eiska bentonitu v stredoslovensk\u00fdch neovulkanitoch<\/strong> – \u0161kolite\u013e Br\u010dekov\u00e1 Jana Klikni pre viac inform\u00e1ci\u00ed<\/span>

Cie\u013eom pr\u00e1ce bude vizualiz\u00e1cia a 3D modelovanie lo\u017eiskov\u00fdch parametrov na z\u00e1klade \u00fadajov z\u00edskan\u00fdch s lo\u017eiskovo-geolick\u00e9ho prieskumu. S\u00fa\u010das\u0165ou pr\u00e1ce bude aj mineralogick\u00e1 a geochemick\u00e1 charakteristika bentonitu vybran\u00fdch vzoriek vrtn\u00e9ho jadra. Na z\u00e1klade korel\u00e1cie v\u00fdsledkov lo\u017eiskovo-geologick\u00fdch \u00fadajov a mineralogicko – geochemick\u00e9ho v\u00fdskumu bud\u00fa upresnen\u00e9 hrance zon\u00e1lnosti bentonitu a n\u00e1sledne modelovan\u00e9 a vizualizovan\u00e9 v GIS a 3D geologickom softv\u00e9ry Leapfrog Geo.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Experiment\u00e1lne, kry\u0161talochemick\u00e9 a spektroskopick\u00e9 \u0161t\u00fadium farebn\u00fdch variet berylu<\/strong> – \u0161kolite\u013e Fridrichov\u00e1 Jana<\/p>\n\n\n\n

K\u00f4rov\u00e9 xenolity v alkalick\u00fdch bazaltoch ju\u017en\u00e9ho Slovenska<\/strong> – \u0161kolite\u013e Monika Huraiov\u00e1 Klikni pre viac inform\u00e1ci\u00ed<\/span>

Mineralogick\u00e1 a petrografick\u00e1 charakteristika xenolitov k\u00f4ry v alkalick\u00fdch bazaltoch ju\u017en\u00e9ho Slovenska.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Charakteristika flu\u00edd s\u00favisiacich s Co-Cu mineraliz\u00e1ciou na na magnezitovo-mastencovom lo\u017eisku Hn\u00fa\u0161\u0165a-M\u00fatnik<\/strong> – \u0161kolite\u013e Peter Kod\u011bra Klikni pre viac inform\u00e1ci\u00ed<\/span>

\u0160t\u00fadium mikrouzavren\u00edn paleoflu\u00edd mikrotermometrick\u00fdmi met\u00f3dami a interpret\u00e1cia \u00fadajov z h\u013eadiska v\u00fdvoja paleoflu\u00edd. \u0160t\u00fadium bude previazan\u00e9 s aktu\u00e1lnym vyh\u013ead\u00e1vac\u00edm prieskumom lo\u017eiska a t\u00e9ma bude rie\u0161en\u00e1 v \u00fazkej spolupr\u00e1ci s prieskumnou firmou.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Hodnotenie dlhodob\u00fdch environment\u00e1lnych riz\u00edk v opusten\u00fdch bansk\u00fdch lokalit\u00e1ch , najm\u00e4 vplyv kysl\u00fdch bansk\u00fdch v\u00f4d na prostredie.<\/strong> – \u0161kolite\u013e Lintnerov\u00e1 Ot\u00edlia<\/p>\n\n\n\n

Po\u010d\u00edta\u010dov\u00e9 modelovanie geologick\u00fdch procesov a jeho vyu\u017eitie v petrol\u00f3gii na pr\u00edklade metamafitov veporika Z\u00e1padn\u00fdch Karp\u00e1t<\/strong> – \u0161kolite\u013e Ondrej Nemec<\/p>\n\n\n\n

Remobiliz\u00e1cia a frakcion\u00e1cia HFS prvkov v granitovom telese Hlohovec-Soro\u0161 v Pova\u017eskom Inovci<\/strong> – \u0161kolite\u013e Martin Ondrejka Klikni pre viac inform\u00e1ci\u00ed<\/span>

V\u00fdskum granitoidn\u00fdch horn\u00edn bratislavsk\u00e9ho hradn\u00e9ho brala s oh\u013eadom na jeho tektonick\u00fa minulos\u0165. Podrobn\u00e9 mapovanie text\u00farnych fenom\u00e9nov pegmatitov\u00fdch a aplitov\u00fdch dajok, tektonick\u00fdch por\u00fach. Mineral\u00f3gia a petrol\u00f3gia magmatick\u00fdch horn\u00edn hradn\u00e9ho brala a ich vz\u0165ah k S-typov\u00fdm granitoidom Bratislavsk\u00e9ho mas\u00edvu.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Petrologicko-tektonick\u00fd v\u00fdskum bratislavsk\u00e9ho hradn\u00e9ho brala<\/strong> – \u0161kolite\u013e Martin Ondrejka Klikni pre viac inform\u00e1ci\u00ed<\/span>

Mineral\u00f3gia a geoch\u00e9mia granitov Pova\u017esk\u00e9ho Inovca v oblasti Hlohovca. Akcesorick\u00e9 miner\u00e1ly prvkov REE, Zr, Hf, Nb, Ta, Th, U a ich altera\u010dn\u00e9 produkty. Mobilita a frakcion\u00e1cia prvkov HFS v prostred\u00ed n\u00edzkych P-T podmienok.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

\u00cdlov\u00e9 miner\u00e1ly v ropn\u00fdch pieskoch z provincie Alberta v Kanade<\/strong> – \u0161kolite\u013e Osack\u00fd Marek Klikni pre viac inform\u00e1ci\u00ed<\/span>

Charakteriz\u00e1cia ropn\u00fdch pieskov z Alberty v Kanade z poh\u013eadu mineral\u00f3gie, chemizmu a povrchov\u00fdch vlastnost\u00ed. D\u00f4raz bude kladen\u00fd na \u0161t\u00fadium \u00edlov a \u00edlov\u00fdch miner\u00e1lov pr\u00edtomn\u00fdch v ropn\u00fdch pieskoch s cie\u013eom lep\u0161ie pochopi\u0165 ich (negat\u00edvny) vplyv na extrakciu bitumenu. Je mo\u017en\u00e1 spolupr\u00e1ca s University of Alberta (Edmonton, Kanada). Pri excelentn\u00fdch v\u00fdsledkoch \u0161tudenta, m\u00f4\u017ee by\u0165 \u0161tudent teoreticky vyslan\u00fd na \u0161tudijn\u00fd pobyt do Kanady (napr. Erasmus?).<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Experiment\u00e1lne \u0161t\u00fadium, mo\u017enosti \u00faprav, stabiliz\u00e1cie a konzerv\u00e1cie miner\u00e1lov a meteoritov v zbierkach m\u00faze\u00ed<\/strong> – \u0161kolite\u013e Ozd\u00edn Daniel<\/p>\n\n\n\n

Petrografia magmatitov a metamorfitov kriedov\u00fdch zlepencov<\/strong> – \u0161kolite\u013e Puti\u0161 Mari\u00e1n<\/p>\n\n\n\n

Mramory a lydity holeck\u00fdch vrstiev betliarskeho s\u00favrstvia gelnickej skupiny ju\u017en\u00e9ho gemerika<\/strong> – \u0161kolite\u013e Ru\u017ei\u010dka Peter<\/p>\n\n\n\n

Petrografia vulkanick\u00e9ho materi\u00e1lu vo v\u00fdplni Dunajskej panvy<\/strong> – \u0161kolite\u013e \u0160arinov\u00e1 Katar\u00edna<\/p>\n\n\n\n

Mo\u017enosti vyu\u017eitia odkaliskov\u00e9ho materi\u00e1lu ako sekund\u00e1rneho zdroja antim\u00f3nu<\/strong> – \u0161kolite\u013e Uhl\u00edk Peter<\/p>\n\n\n\n

Nb-Ta miner\u00e1ly v leukogranitoch gemerika<\/strong> – \u0161kolite\u013e Uher Pavel<\/p>\n\n\n\n

Distrib\u00facia prvkov vz\u00e1cnych zem\u00edn (REE) vo vybran\u00fdch fosf\u00e1tov\u00fdch biominer\u00e1loch<\/strong> – \u0161kolite\u013e Pavel Uher Klikni pre viac inform\u00e1ci\u00ed<\/span>

\u0160t\u00fadium koncentr\u00e1cie prvkov vz\u00e1cnych zem\u00edn (REE) a \u010fal\u0161\u00edch prvkov na pr\u00edkladoch fos\u00edlnych bioapatitov (najm\u00e4 fosilizovan\u00e9 kosti r\u00f4znych foriem Vertebrata) z r\u00f4znych geologick\u00fdch obdob\u00ed (paleozoikum a\u017e pleistoc\u00e9n) s vyu\u017eit\u00edm mikroanalytick\u00fdch in-situ met\u00f3d (EPMA, LA ICP MS). Interpret\u00e1cia mechanizmu vstupu REE do fos\u00edlnych bioapatitov.<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Petrol\u00f3gia meta-magmatitov star\u0161ieho paleozoika veporika alebo gemerika<\/strong> – \u0161kolite\u013e Mari\u00e1n Puti\u0161 Klikni pre viac inform\u00e1ci\u00ed<\/span>

Charakteristika magmatizmu a metamorf\u00f3zy; reko\u0161trukcia v\u00fdvoja (ter\u00e9n, mikroskopia, pr\u00edprava vzoriek na petrologicko-geochemick\u00fd v\u00fdskum, pr\u00edp. geochronologiu; aplik\u00e1cia EPMA, LA-ICP-MS, ICP-MS)<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n

Mineral\u00f3gia, hydroterm\u00e1lne premeny a vlastnosti paleoflu\u00edd Au-Ag epiterm\u00e1lnych \u017e\u00edl v prieskumn\u00fdch vrtoch v Andrej \u0161t\u00f4lni v Kremnici<\/strong> – \u0161kolite\u013e Kod\u011bra Peter Klikni pre viac inform\u00e1ci\u00ed<\/span>

Komplexn\u00e1 charakteriz\u00e1cia drahokovovej \u017eilnej mineraliz\u00e1cie vo vrtoch aktu\u00e1lneho vrtn\u00e9ho prieskumu firmy Metaltech, realizovanom v Andrej \u0161t\u00f4lni v Kremnici<\/span><\/p>\n\n\n\n<\/div>\n\n\n\n
\n\n\n\n

Dizerta\u010dn\u00e9 pr\u00e1ce<\/span><\/h2>\n\n\n\n

Akademick\u00fd rok 2025\/2026<\/h4>\n\n\n\n
T\u00e9ma<\/td>anot\u00e1cia<\/td>\u0160kolite\u013e<\/td>Pracovisko<\/td>Forma \u0161t\u00fadia<\/td><\/tr>
Later\u00e1lne a vertik\u00e1lne pr\u00fadenie flu\u00edd v porf\u00fdrov\u00fdch a epiterm\u00e1lnych syst\u00e9moch<\/td>Porfyrov\u00e9 a epiterm\u00e1lne lo\u017eisk\u00e1 s\u00fa v\u00fdznamn\u00fdm potenci\u00e1lnym zdrojom kritick\u00fdch a strategick\u00fdch nerastn\u00fdch surov\u00edn, ak\u00fdmi s\u00fa Cu, Mo, W a Au. Pr\u00fadenie hydroterm\u00e1lnych flu\u00edd v porf\u00fdrov\u00fdch syst\u00e9moch je zvy\u010dajne vertik\u00e1lne smerom nahor od zdroja tepla\/flu\u00edd, ale akon\u00e1hle fluidum dosiahne plyt\u0161ie \u00farovne a\/alebo heterogenity v priepustnosti (zlomy, nepriepustn\u00e9 alebo reakt\u00edvne horniny), m\u00f4\u017ee tie\u017e migrova\u0165 later\u00e1lne a sp\u00f4sobi\u0165 tvorbu r\u00f4znych typov satelitn\u00fdch alebo epiterm\u00e1lnych mineraliz\u00e1ci\u00ed. Pr\u00fadenie flu\u00edd do zna\u010dnej miery z\u00e1vis\u00ed od \u0161trukt\u00farnych heterogen\u00edt a reakci\u00ed fluidum-hornina, ktor\u00e9 m\u00f4\u017eu akt\u00edvne meni\u0165 priepustnos\u0165. Cesty flu\u00edd mo\u017eno rozpozna\u0165 na z\u00e1klade zmien v zlo\u017een\u00ed vykry\u0161talizovan\u00fdch miner\u00e1lov a miner\u00e1lnych asoci\u00e1ci\u00ed , distrib\u00facie alter\u00e1ci\u00ed a vlastnost\u00ed paleoflu\u00edd, ktor\u00e9 mo\u017eno sledova\u0165 anal\u00fdzami fluidn\u00fdch inkl\u00fazi\u00ed a stabiln\u00fdch izotopov, ako aj miner\u00e1lnou termometriou. T\u00e1to t\u00e9ma bude sk\u00faman\u00e1 na slovensk\u00fdch rudn\u00fdch lo\u017eisk\u00e1ch a prieskumn\u00fdch \u00fazemiach, ktor\u00e9 s\u00fa v poslednom obdob\u00ed predmetom intenz\u00edvneho prieskumu a v\u00fdskumu, s dostato\u010dnou \u00farov\u0148ou vedomost\u00ed a dostupnos\u0165ou vzoriek z r\u00f4znych \u010dast\u00ed a \u00farovn\u00ed syst\u00e9mov. GIS programy bud\u00fa pou\u017eit\u00e9 na priestorov\u00fa vizualiz\u00e1ciu interpret\u00e1cie star\u0161\u00edch a nov\u00fdch analytick\u00fdch, geologick\u00fdch a \u0161trukt\u00farnych \u00fadajov. Cie\u013eom \u0161t\u00fadia je definovanie hlavn\u00fdch faktorov pr\u00fadenia hydroterm\u00e1lnych flu\u00edd, ktor\u00e9 ved\u00fa k hydroterm\u00e1lnemu obohacovaniu a frakciona\u010dn\u00fdm procesom zodpovedn\u00fdm za tvorbu porf\u00fdrov\u00fdch a epiterm\u00e1lnych lo\u017e\u00edsk.<\/td>prof. Mgr. Peter Kod\u011bra, PhD.<\/td>PriF<\/td>denn\u00e1<\/td><\/tr>
Vplyv jednotliv\u00fdch vlastnost\u00ed ropn\u00fdch pieskov na extrakciu bitum\u00e9nu<\/td>Lo\u017eisko ropn\u00fdch pieskov v Alberte predstavuje v\u00fdznamn\u00fd zdroj ropy na plan\u00e9te. Hoci je zn\u00e1mych ve\u013ea faktorov ovplyv\u0148uj\u00facich extrakciu bitumenu, st\u00e1le nie je jasn\u00e9, ktor\u00e9 faktory s\u00fa k\u013e\u00fa\u010dov\u00e9 a ktor\u00e9 s\u00fa menej d\u00f4le\u017eit\u00e9. Sk\u00fama\u0165 sa bud\u00fa umelo pripraven\u00e9 miner\u00e1lne zmesi, ktor\u00e9 svojim zlo\u017een\u00edm bud\u00fa simulova\u0165 zlo\u017eenie pr\u00edrodn\u00fdch ropn\u00fdch pieskov. Nadobudnut\u00e9 v\u00fdsledky umo\u017enia lep\u0161ie pochopi\u0165 mieru vplyvu jednotliv\u00fdch parametrov ropn\u00fdch pieskov (mineral\u00f3gia, chemizmus, povrchov\u00e9 vlastnosti) na extrakciu bitumenu.  Jedn\u00fdm z d\u00f4le\u017eit\u00fdch v\u00fdstupov pre ropn\u00e9 spolo\u010dnosti bude lep\u0161ia predikcia mno\u017estva extrahovan\u00e9ho bitumenu z r\u00f4znych typov ropn\u00fdch pieskov. <\/td>doc. Mgr. Marek Osack\u00fd, PhD.<\/td>PriF<\/td>denn\u00e1<\/td><\/tr>
\u00cdlov\u00e9 suroviny ako doplnkov\u00fd cementov\u00fd materi\u00e1l<\/td>V\u00fdrobky na b\u00e1ze cementu (30 mili\u00e1rd ton bet\u00f3nu, malty at\u010f. ro\u010dne) s\u00fa v\u010faka svojim vynikaj\u00facim vlastnostiam, miestnej dostupnosti surov\u00edn a cene najspotrebovanej\u0161\u00edm vyr\u00e1ban\u00fdm materi\u00e1lom na svete. Nev\u00fdhodou t\u00fdchto materi\u00e1lov je vplyv na \u017eivotn\u00e9 prostredie. Pri v\u00fdrobe 1 tony slinku sa uvo\u013en\u00ed asi 875 kg oxidu uhli\u010dit\u00e9ho (CO2), z \u010doho 60 % poch\u00e1dza z v\u00e1penca a zvy\u0161n\u00fdch 40 % poch\u00e1dza z energie potrebnej na proces. Aj ke\u010f je mno\u017estvo emitovan\u00e9ho CO2 na jednotku hmotnosti v porovnan\u00ed s in\u00fdmi vyr\u00e1ban\u00fdmi materi\u00e1lmi mal\u00e9, enormn\u00e1 produkcia sp\u00f4sobuje, \u017ee cement\u00e1rensk\u00fd priemysel v s\u00fa\u010dasnosti predstavuje pribli\u017ene 7 % celosvetov\u00fdch emisi\u00ed CO2 a glob\u00e1lny dopyt sa bude zvy\u0161ova\u0165. Naj\u00fa\u010dinnej\u0161\u00edm a najhospod\u00e1rnej\u0161\u00edm n\u00e1strojom na dekarboniz\u00e1ciu v cement\u00e1rskom priemysle sa jav\u00ed \u010diasto\u010dn\u00e1 n\u00e1hrada slinku alebo cementu doplnkov\u00fdmi cementov\u00fdmi materi\u00e1lmi (supplementary cementitious materials SCMs). Jedn\u00fdm s najperspekt\u00edvnej\u0161\u00edm SCM s\u00fa \u00edlov\u00e9 suroviny, pre ich dostupnos\u0165 a vhodn\u00e9 fyzik\u00e1lno-mechanick\u00e9 vlastnosti na z\u00e1klade doteraz publikovan\u00fdch pr\u00e1c. Potreba v\u00fdskumu \u00edlov\u00fdch surov\u00edn ako SCM je nevyhnutn\u00e1 pre pochopenie reakcii medzi cementov\u00fdmi f\u00e1zami a aluminosilik\u00e1tov\u00fdmi f\u00e1zami z \u00edlov\u00fdch surov\u00edn. Z\u00e1rove\u0148 ka\u017ed\u00e9 lo\u017eisko ilovej suroviny je \u0161pecifick\u00e9.<\/td>doc. Mgr. Peter Uhl\u00edk, PhD.<\/td>PriF<\/td>denn\u00e1<\/td><\/tr>
Geoch\u00e9mia fylosilik\u00e1tov ako n\u00e1stroj na prieskum v hydroterm\u00e1lnom prostred\u00ed<\/td>Reakt\u00edvne fluid\u00e1, ktor\u00e9 s\u00fa pod tlakom sp\u00f4sobuj\u00fa v porf\u00fdrov\u00fdch syst\u00e9moch tvorbu \u017e\u00edl a \u017eiln\u00edkov, a rozsiahle alter\u00e1cie sprievodn\u00fdch horn\u00edn, pri\u010dom vznikaj\u00fa fylosilik\u00e1ty, ktor\u00e9 reaguj\u00fa na zmeny v chemizme prostredia a m\u00f4\u017eu by\u0165 pou\u017eit\u00e9 ako indik\u00e1tory procesov ved\u00facich k ukladaniu rudy. Pokro\u010dil\u00e9 analytick\u00e9 met\u00f3dy umo\u017e\u0148uj\u00fa pou\u017ei\u0165 stopov\u00e9 prvky v altera\u010dn\u00fdch miner\u00e1loch na smerovanie prieskumu. T\u00e1to pr\u00e1ca bude \u0161tudova\u0165 vzorky z dobre definovan\u00fdch porf\u00fdrov\u00fdch a epiterm\u00e1lnych lo\u017e\u00edsk na Slovensku s mo\u017enos\u0165ou porovnania \u00fadajov s v\u00fdsledkami in\u00fdch nez\u00e1visl\u00fdch met\u00f3d. Pre porovnanie s in\u00fdmi prieskumn\u00fdmi n\u00e1strojmi bud\u00fa zahrnut\u00e9 aj lokality, kde prebieha aktu\u00e1lny prieskum. S\u00fa\u010dasne podrobn\u00e1 geochemick\u00e1 \u0161t\u00fadia \u00edlov\u00fdch miner\u00e1lov a in\u00fdch fylosilik\u00e1tov m\u00f4\u017ee tie\u017e poskytn\u00fa\u0165 poh\u013ead na procesy, ktor\u00e9 sp\u00f4sobuj\u00fa obohatenie kovmi (napr. prvok vz\u00e1cnych zem\u00edn (REE) a in\u00e9) v \u00edlovej frakcii.<\/td>doc. Mgr. Peter Uhl\u00edk, PhD.<\/td>PriF<\/td>denn\u00e1<\/td><\/tr>
Leukogranity a granitov\u00e9 pegmatity veporika: mineralogicko-geochemick\u00e1 charakteristika a evol\u00facia<\/td>Z\u00e1kladn\u00e1 geologick\u00e1, geochemick\u00e1 a najm\u00e4 mineralogick\u00e1 charakteristika varisk\u00fdch leukokr\u00e1tnych granitov a granitov\u00fdch pegmatitov vo veporiku, ich vz\u00e1jomn\u00e9 genetick\u00e9 vz\u0165ahy. Pr\u00e1ca zah\u0155\u0148a ter\u00e9nny v\u00fdskum, odber vzoriek a ich laborat\u00f3rne spracovanie (najm\u00e4 elektr\u00f3nov\u00e1 mikrosonda, anal\u00fdzy horn\u00edn a datovanie miner\u00e1lov). Na z\u00e1klade analytick\u00fdch \u00fadajov bude vytvoren\u00fd petrogenetick\u00fd model evol\u00facie leukogranitov a pegmatitov.<\/td>prof. RNDr. Pavel Uher, CSc.<\/td>PriF<\/td>denn\u00e1<\/td><\/tr>
Vulkanoklastick\u00fd materi\u00e1l vo v\u00fdplni neog\u00e9nnych paniev – tefrostratigrafia, ekonomick\u00fd potenci\u00e1l<\/td>Datovanie pyrokastick\u00fdch horn\u00edn, porovn\u00e1vanie pyrokast\u00edk z r\u00f4znych lokal\u00edt na z\u00e1klade chemick\u00fdch signat\u00far a indexov\u00fdch miner\u00e1lov ako podklad pre tefrostratigrafiu neog\u00e9nnych paniev. Sk\u00famanie  altera\u010dn\u00fdch produktov z h\u013eadiska diagen\u00e9zy a ekonomick\u00e9ho vyu\u017eitia.<\/td>doc. Mgr. Katar\u00edna \u0160arinov\u00e1, PhD.<\/td>PriF<\/td>denn\u00e1<\/td><\/tr>
Megakry\u0161t\u00e1ly a produkty ich rozpadu v alkalick\u00fdch bazaltoch ju\u017en\u00e9ho Slovenska: mineral\u00f3gia a gen\u00e9za.<\/td>Systematick\u00e9 mineralogick\u00e9 \u0161t\u00fadium megakry\u0161t\u00e1lov so zameran\u00edm na gen\u00e9zu klinopyrox\u00e9nu, plagioklasu a pseudomorf\u00f3z po rozpade amfibolu. Meranie obsahu vodu pomocou infra\u010dervenej spetroskopie. Termobarometria plagioklas-tavenina a pyrox\u00e9n-tavenina. Interakcia s bazaltom. Termodynamick\u00e9 modelovanie. <\/td>prof. RNDr. Monika Huraiov\u00e1, PhD.<\/td>PriF<\/td>denn\u00e1<\/td><\/tr>
Leukogranity a granitov\u00e9 pegmatity z\u00e1padnej \u010dasti tatrika: mineralogicko-geochemick\u00e1 charakteristika a evol\u00facia<\/td>Z\u00e1kladn\u00e1 geologick\u00e1, geochemick\u00e1 a najm\u00e4 mineralogick\u00e1 charakteristika varisk\u00fdch leukokr\u00e1tnych granitov a granitov\u00fdch pegmatitov vo z\u00e1padnej \u010dasti tatrika (M. Karpaty, Pov. Inovec, Tribe\u010d, Str\u00e1\u017eovsk\u00e9 vrchy), ich vz\u00e1jomn\u00e9 genetick\u00e9 vz\u0165ahy. Pr\u00e1ca zah\u0155\u0148a ter\u00e9nny v\u00fdskum, odber vzoriek a ich laborat\u00f3rne spracovanie (najm\u00e4 elektr\u00f3nov\u00e1 mikrosonda, anal\u00fdzy horn\u00edn a datovanie miner\u00e1lov). Na z\u00e1klade analytick\u00fdch \u00fadajov bude vytvoren\u00fd petrogenetick\u00fd model evol\u00facie leukogranitov a pegmatitov.<\/td>prof. RNDr. Pavel Uher, CSc.<\/td>PriF<\/td>denn\u00e1<\/td><\/tr>
Petrol\u00f3gia a geoch\u00e9mia metamagmatitov a metasedimentov v sut\u00farnych z\u00f3nach orog\u00e9nov<\/td>Ter\u00e9nne \u0161t\u00fadium suturn\u00fdch z\u00f3n. Petrografia, chemizmus miner\u00e1lov a horn\u00edn, izotopick\u00e9 \u0161t\u00fadium, geochronol\u00f3gia, P-T-X podmienky magmatickej a metamorfnej etapy v\u00fdvoja, spracovanie d\u00e1t a petrogenetick\u00e1 interpret\u00e1cia.<\/td>prof. RNDr. Mari\u00e1n Puti\u0161, DrSc.<\/td>PriF<\/td>denn\u00e1<\/td><\/tr>
Evalu\u00e1cia \u00edlov\u00fdch surov\u00edn Slovenska na v\u00fdrobu keramick\u00fdch prefabrikovan\u00fdch materi\u00e1lov<\/td>Pos\u00fadenie vhodnosti \u00edlov\u00fdch surov\u00edn Slovenska pre v\u00fdrobu keramick\u00fdch prefabrikovan\u00fdch materi\u00e1lov. Z datab\u00e1zy \u00edlov\u00fdch surov\u00edn z r\u00f4znych lo\u017e\u00edsk na \u00fazem\u00ed Slovenska bud\u00fa vytipovan\u00e9 na z\u00e1klade r\u00f4znych vlastnost\u00ed (miner\u00e1lne zlo\u017eenie, fyzik\u00e1lne a chemick\u00e9 vlastnosti) vhodn\u00e9 suroviny, ktor\u00e9 sa pou\u017eij\u00fa na v\u00fdrobu keramick\u00e9ho prefabrik\u00e1tu (keramzitu) v laborat\u00f3rnych podmienkach. Na vyrobenom keramzite sa stanov\u00ed miner\u00e1lne a chemick\u00e9 zlo\u017eenie pomocou \u0161tandardn\u00fdch mineralogick\u00fdch analytick\u00fdch met\u00f3d (XRD, SEM, Raman). N\u00e1sledne bud\u00fa fyzik\u00e1lne, mechanick\u00e9 a statick\u00e9 vlastnosti v\u00fdrobku testovan\u00e9 v stavebn\u00fdch laborat\u00f3riach, kde sa over\u00ed ich vhodnos\u0165 pre pou\u017eitie v stavebnej praxi.<\/td>doc. RNDr. Jana Fridrichov\u00e1, PhD.<\/td>PriF<\/td>denn\u00e1<\/td><\/tr>
Mineralogick\u00fd v\u00fdskum miner\u00e1lov turmal\u00ednovej superskupiny v pegmatitoch Kru\u0161n\u00fdch Hor (\u010cesk\u00e1 republika)<\/td>Mineralogick\u00fd v\u00fdskum miner\u00e1lov turmal\u00ednovej superskupiny sa bude sklada\u0165 s kry\u0161talochemick\u00e9ho a genetick\u00e9ho v\u00fdskumu r\u00f4znych typov a zlo\u017een\u00ed turmal\u00ednov na pegmatitoch Kru\u0161n\u00fdch Hor (napr. lokalita Smoln\u00e9 Pece) prostredn\u00edctvom pestr\u00e9ho spektra analytick\u00fdch met\u00f3d (EMPA, LA-ICP-MS, PXRD, SREF, FTIR, Raman, OAS, M\u00f6ssbauer).<\/td>doc. RNDr. Peter Ba\u010d\u00edk, PhD.<\/td>PriF<\/td>denn\u00e1<\/td><\/tr>
Vyu\u017eitie v\u00e4zbovej topol\u00f3gie na rie\u0161enie \u0161trukt\u00farnych efektov substit\u00faci\u00ed v silik\u00e1toch<\/td>V r\u00e1mci tohto v\u00fdskumu bude vyu\u017eit\u00fd v\u00e4zbov\u00fd topologick\u00fd model na predpovedanie \u0161trukt\u00farnej stability silik\u00e1tov, odha\u013eovanie a interpret\u00e1ciu kry\u0161talochemick\u00fdch procesov vyskytuj\u00facich sa v re\u00e1lnych \u0161trukt\u00farach a navrhovanie mo\u017en\u00fdch zmien miner\u00e1lnej \u0161trukt\u00fary a zlo\u017eenia.<\/td>doc. RNDr. Peter Ba\u010d\u00edk, PhD.<\/td>PriF<\/td>denn\u00e1<\/td><\/tr>
Zvetr\u00e1vanie miner\u00e1lov tetraedritovej skupiny: mobilita prvkov a superg\u00e9nne produkty<\/td>Detailn\u00e9 \u0161t\u00fadium chemick\u00e9ho zlo\u017eenia prim\u00e1rnych\/nealterovan\u00fdch miner\u00e1lov tetraedritovej skupiny, identifik\u00e1ciu a pokro\u010dil\u00fd kry\u0161talochemick\u00fd v\u00fdskum v\u0161etk\u00fdch superg\u00e9nnych produktov zvetr\u00e1vania a stanovenie geochemick\u00e9ho spr\u00e1vania a mobility toxick\u00fdch prvkov po\u010das zvetr\u00e1vania miner\u00e1lov tetraedritovej skupiny<\/td>Mgr. Martin \u0160tevko, PhD.<\/td>SAV<\/td>denn\u00e1<\/td><\/tr>
Organick\u00e1 petrografia: Aplik\u00e1cie v paleoekol\u00f3gii, geohist\u00f3rii, energetick\u00fdch zdrojoch a archeol\u00f3gii<\/td>V\u00fdskum organickej hmoty v hornin\u00e1ch a sedimentoch pon\u00faka jedine\u010dn\u00fa pr\u00edle\u017eitos\u0165 analyzova\u0165 fascinuj\u00face pr\u00edrodn\u00e9 a kult\u00farne fenom\u00e9ny, ktor\u00e9 sa vyskytli v hist\u00f3rii Zeme a \u013eudskej civiliz\u00e1cie. Aplik\u00e1cia organickej petrografie na jazern\u00e9 a morsk\u00e9 sedimenty umo\u017en\u00ed hlb\u0161ie pochopi\u0165 klimatick\u00e9 a ekologick\u00e9 zmeny, ako aj geologick\u00e9 procesy spojen\u00e9 s term\u00e1lnou hist\u00f3riou horn\u00edn, formovan\u00edm, migr\u00e1ciou a akumul\u00e1ciou ropy a zemn\u00e9ho plynu. V\u00fdskum bude zah\u0155\u0148a\u0165 aj anal\u00fdzu paleopo\u017eiarov. Na z\u00e1klade teploty horenia a typov sp\u00e1len\u00fdch \u010dast\u00edc sa z\u00edskaj\u00fa cenn\u00e9 inform\u00e1cie o charaktere veget\u00e1cie a koncentr\u00e1cii kysl\u00edka v r\u00f4znych obdobiach hist\u00f3rie Zeme.<\/td>RNDr. J\u00falia Kotulov\u00e1, PhD.<\/td>SAV<\/td>denn\u00e1<\/td><\/tr>
Leukogranity a granitov\u00e9 pegmatity veporika: mineralogicko-geochemick\u00e1 charakteristika a evol\u00facia<\/td>Z\u00e1kladn\u00e1 geologick\u00e1, geochemick\u00e1 a najm\u00e4 mineralogick\u00e1 charakteristika varisk\u00fdch leukokr\u00e1tnych granitov a granitov\u00fdch pegmatitov vo veporiku, ich vz\u00e1jomn\u00e9 genetick\u00e9 vz\u0165ahy. Pr\u00e1ca zah\u0155\u0148a ter\u00e9nny v\u00fdskum, odber vzoriek a ich laborat\u00f3rne spracovanie (najm\u00e4 elektr\u00f3nov\u00e1 mikrosonda, anal\u00fdzy horn\u00edn a datovanie miner\u00e1lov). Na z\u00e1klade analytick\u00fdch \u00fadajov bude vytvoren\u00fd petrogenetick\u00fd model evol\u00facie leukogranitov a pegmatitov.<\/td>prof. RNDr. Pavel Uher, CSc.<\/td>PriF<\/td>extern\u00e1<\/td><\/tr>
Leukogranity a granitov\u00e9 pegmatity z\u00e1padnej \u010dasti tatrika: mineralogicko-geochemick\u00e1 charakteristika a evol\u00facia<\/td>Z\u00e1kladn\u00e1 geologick\u00e1, geochemick\u00e1 a najm\u00e4 mineralogick\u00e1 charakteristika varisk\u00fdch leukokr\u00e1tnych granitov a granitov\u00fdch pegmatitov vo z\u00e1padnej \u010dasti tatrika (M. Karpaty, Pov. Inovec, Tribe\u010d, Str\u00e1\u017eovsk\u00e9 vrchy), ich vz\u00e1jomn\u00e9 genetick\u00e9 vz\u0165ahy. Pr\u00e1ca zah\u0155\u0148a ter\u00e9nny v\u00fdskum, odber vzoriek a ich laborat\u00f3rne spracovanie (najm\u00e4 elektr\u00f3nov\u00e1 mikrosonda, anal\u00fdzy horn\u00edn a datovanie miner\u00e1lov). Na z\u00e1klade analytick\u00fdch \u00fadajov bude vytvoren\u00fd petrogenetick\u00fd model evol\u00facie leukogranitov a pegmatitov.<\/td>prof. RNDr. Pavel Uher, CSc.<\/td>PriF<\/td>extern\u00e1<\/td><\/tr>
Organick\u00e1 petrografia: Aplik\u00e1cie v paleoekol\u00f3gii, geohist\u00f3rii, energetick\u00fdch zdrojoch a archeol\u00f3gii<\/td>V\u00fdskum organickej hmoty v hornin\u00e1ch a sedimentoch pon\u00faka jedine\u010dn\u00fa pr\u00edle\u017eitos\u0165 analyzova\u0165 fascinuj\u00face pr\u00edrodn\u00e9 a kult\u00farne fenom\u00e9ny, ktor\u00e9 sa vyskytli v hist\u00f3rii Zeme a \u013eudskej civiliz\u00e1cie. Aplik\u00e1cia organickej petrografie na jazern\u00e9 a morsk\u00e9 sedimenty umo\u017en\u00ed hlb\u0161ie pochopi\u0165 klimatick\u00e9 a ekologick\u00e9 zmeny, ako aj geologick\u00e9 procesy spojen\u00e9 s term\u00e1lnou hist\u00f3riou horn\u00edn, formovan\u00edm, migr\u00e1ciou a akumul\u00e1ciou ropy a zemn\u00e9ho plynu. V\u00fdskum bude zah\u0155\u0148a\u0165 aj anal\u00fdzu paleopo\u017eiarov. Na z\u00e1klade teploty horenia a typov sp\u00e1len\u00fdch \u010dast\u00edc sa z\u00edskaj\u00fa cenn\u00e9 inform\u00e1cie o charaktere veget\u00e1cie a koncentr\u00e1cii kysl\u00edka v r\u00f4znych obdobiach hist\u00f3rie Zeme.<\/td>RNDr. J\u00falia Kotulov\u00e1, PhD.<\/td>SAV<\/td>extern\u00e1<\/td><\/tr><\/tbody><\/table><\/figure>\n","protected":false},"excerpt":{"rendered":"

Zvo\u013e typ z\u00e1vere\u010dnej pr\u00e1ce Bakal\u00e1rske pr\u00e1ce 2019\/2020 Mineralogick\u00e1 a genetick\u00e1 … <\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0,"ngg_post_thumbnail":0},"folder":[49],"yoast_head":"\nT\u00e9my z\u00e1vere\u010dn\u00fdch pr\u00e1c - Katedra mineral\u00f3gie, petrol\u00f3gie a lo\u017eiskovej geol\u00f3gie<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/kmplg.sk\/?page_id=85\" \/>\n<meta property=\"og:locale\" content=\"sk_SK\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"T\u00e9my z\u00e1vere\u010dn\u00fdch pr\u00e1c - Katedra mineral\u00f3gie, petrol\u00f3gie a lo\u017eiskovej geol\u00f3gie\" \/>\n<meta property=\"og:description\" content=\"Zvo\u013e typ z\u00e1vere\u010dnej pr\u00e1ce Bakal\u00e1rske pr\u00e1ce 2019\/2020 Mineralogick\u00e1 a genetick\u00e1 …\" \/>\n<meta property=\"og:url\" content=\"https:\/\/kmplg.sk\/?page_id=85\" \/>\n<meta property=\"og:site_name\" content=\"Katedra mineral\u00f3gie, petrol\u00f3gie a lo\u017eiskovej geol\u00f3gie\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/kmplg\/\" \/>\n<meta property=\"article:modified_time\" content=\"2025-02-24T08:56:43+00:00\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Predpokladan\u00fd \u010das \u010d\u00edtania\" \/>\n\t<meta name=\"twitter:data1\" content=\"16 min\u00fat\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"WebSite\",\"@id\":\"https:\/\/kmplg.sk\/#website\",\"url\":\"https:\/\/kmplg.sk\/\",\"name\":\"Katedra mineral\u00f3gie, petrol\u00f3gie a lo\u017eiskovej geol\u00f3gie\",\"description\":\"Pr\u00edrodovedeck\u00e1 fakulta Univerzity Komensk\u00e9ho v Bratislave\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\/\/kmplg.sk\/?s={search_term_string}\"},\"query-input\":\"required name=search_term_string\"}],\"inLanguage\":\"sk-SK\"},{\"@type\":\"WebPage\",\"@id\":\"https:\/\/kmplg.sk\/?page_id=85\",\"url\":\"https:\/\/kmplg.sk\/?page_id=85\",\"name\":\"T\u00e9my z\u00e1vere\u010dn\u00fdch pr\u00e1c - Katedra mineral\u00f3gie, petrol\u00f3gie a lo\u017eiskovej geol\u00f3gie\",\"isPartOf\":{\"@id\":\"https:\/\/kmplg.sk\/#website\"},\"datePublished\":\"2021-03-05T05:34:48+00:00\",\"dateModified\":\"2025-02-24T08:56:43+00:00\",\"breadcrumb\":{\"@id\":\"https:\/\/kmplg.sk\/?page_id=85#breadcrumb\"},\"inLanguage\":\"sk-SK\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\/\/kmplg.sk\/?page_id=85\"]}]},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\/\/kmplg.sk\/?page_id=85#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"https:\/\/kmplg.sk\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"T\u00e9my z\u00e1vere\u010dn\u00fdch pr\u00e1c\"}]}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"T\u00e9my z\u00e1vere\u010dn\u00fdch pr\u00e1c - Katedra mineral\u00f3gie, petrol\u00f3gie a lo\u017eiskovej geol\u00f3gie","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/kmplg.sk\/?page_id=85","og_locale":"sk_SK","og_type":"article","og_title":"T\u00e9my z\u00e1vere\u010dn\u00fdch pr\u00e1c - Katedra mineral\u00f3gie, petrol\u00f3gie a lo\u017eiskovej geol\u00f3gie","og_description":"Zvo\u013e typ z\u00e1vere\u010dnej pr\u00e1ce Bakal\u00e1rske pr\u00e1ce 2019\/2020 Mineralogick\u00e1 a genetick\u00e1 …","og_url":"https:\/\/kmplg.sk\/?page_id=85","og_site_name":"Katedra mineral\u00f3gie, petrol\u00f3gie a lo\u017eiskovej geol\u00f3gie","article_publisher":"https:\/\/www.facebook.com\/kmplg\/","article_modified_time":"2025-02-24T08:56:43+00:00","twitter_card":"summary_large_image","twitter_misc":{"Predpokladan\u00fd \u010das \u010d\u00edtania":"16 min\u00fat"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebSite","@id":"https:\/\/kmplg.sk\/#website","url":"https:\/\/kmplg.sk\/","name":"Katedra mineral\u00f3gie, petrol\u00f3gie a lo\u017eiskovej geol\u00f3gie","description":"Pr\u00edrodovedeck\u00e1 fakulta Univerzity Komensk\u00e9ho v Bratislave","potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/kmplg.sk\/?s={search_term_string}"},"query-input":"required name=search_term_string"}],"inLanguage":"sk-SK"},{"@type":"WebPage","@id":"https:\/\/kmplg.sk\/?page_id=85","url":"https:\/\/kmplg.sk\/?page_id=85","name":"T\u00e9my z\u00e1vere\u010dn\u00fdch pr\u00e1c - Katedra mineral\u00f3gie, petrol\u00f3gie a lo\u017eiskovej geol\u00f3gie","isPartOf":{"@id":"https:\/\/kmplg.sk\/#website"},"datePublished":"2021-03-05T05:34:48+00:00","dateModified":"2025-02-24T08:56:43+00:00","breadcrumb":{"@id":"https:\/\/kmplg.sk\/?page_id=85#breadcrumb"},"inLanguage":"sk-SK","potentialAction":[{"@type":"ReadAction","target":["https:\/\/kmplg.sk\/?page_id=85"]}]},{"@type":"BreadcrumbList","@id":"https:\/\/kmplg.sk\/?page_id=85#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"https:\/\/kmplg.sk\/"},{"@type":"ListItem","position":2,"name":"T\u00e9my z\u00e1vere\u010dn\u00fdch pr\u00e1c"}]}]}},"_links":{"self":[{"href":"https:\/\/kmplg.sk\/index.php?rest_route=\/wp\/v2\/pages\/85"}],"collection":[{"href":"https:\/\/kmplg.sk\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/kmplg.sk\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/kmplg.sk\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/kmplg.sk\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=85"}],"version-history":[{"count":5,"href":"https:\/\/kmplg.sk\/index.php?rest_route=\/wp\/v2\/pages\/85\/revisions"}],"predecessor-version":[{"id":3397,"href":"https:\/\/kmplg.sk\/index.php?rest_route=\/wp\/v2\/pages\/85\/revisions\/3397"}],"wp:attachment":[{"href":"https:\/\/kmplg.sk\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=85"}],"wp:term":[{"taxonomy":"folder","embeddable":true,"href":"https:\/\/kmplg.sk\/index.php?rest_route=%2Fwp%2Fv2%2Ffolder&post=85"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}