{"id":72044,"date":"2024-09-27T10:24:36","date_gmt":"2024-09-27T09:24:36","guid":{"rendered":"https:\/\/www.upjs.sk\/prirodovedecka-fakulta\/?post_type=cpt_aktualne_spravy&#038;p=72044"},"modified":"2024-10-08T15:32:52","modified_gmt":"2024-10-08T14:32:52","slug":"inovativne-3d-modelovanie-mineralnych-zrn-odhaluje-geologicku-minulost","status":"publish","type":"cpt_aktuality","link":"https:\/\/www.upjs.sk\/prirodovedecka-fakulta\/actuality\/inovativne-3d-modelovanie-mineralnych-zrn-odhaluje-geologicku-minulost\/","title":{"rendered":"Inovat\u00edvne 3D modelovanie miner\u00e1lnych z\u0155n odha\u013euje geologick\u00fa minulos\u0165"},"content":{"rendered":"<style>.kadence-column72044_68f388-92 > .kt-inside-inner-col{padding-top:var(--global-kb-spacing-xs, 1rem);padding-right:var(--global-kb-spacing-xs, 1rem);padding-left:var(--global-kb-spacing-xs, 1rem);}.kadence-column72044_68f388-92 > .kt-inside-inner-col,.kadence-column72044_68f388-92 > .kt-inside-inner-col:before{border-top-left-radius:5px;border-top-right-radius:5px;border-bottom-right-radius:5px;border-bottom-left-radius:5px;}.kadence-column72044_68f388-92 > .kt-inside-inner-col{column-gap:var(--global-kb-gap-sm, 1rem);}.kadence-column72044_68f388-92 > .kt-inside-inner-col{flex-direction:column;}.kadence-column72044_68f388-92 > .kt-inside-inner-col > .aligncenter{width:100%;}.kadence-column72044_68f388-92 > .kt-inside-inner-col{background-color:#F4F4F4;}.kadence-column72044_68f388-92 > .kt-inside-inner-col:before{opacity:0.3;}.kadence-column72044_68f388-92{position:relative;}@media all and (max-width: 1024px){.kadence-column72044_68f388-92 > .kt-inside-inner-col{flex-direction:column;}}@media all and (max-width: 767px){.kadence-column72044_68f388-92 > .kt-inside-inner-col{flex-direction:column;}}<\/style>\n<div class=\"wp-block-kadence-column kadence-column72044_68f388-92\"><div class=\"kt-inside-inner-col\">\n<p class=\"has-text-align-justify\">V\u00fdskumn\u00fd t\u00edm <a href=\"https:\/\/www.upjs.sk\/PF\/zamestnanec\/katarina.bonova\/\">docentky Katar\u00edny B\u00f3novej<\/a> z <a href=\"https:\/\/www.upjs.sk\/prirodovedecka-fakulta\/pracoviska\/ustavy-pf\/uge\/\">\u00dastavu geografie<\/a> na Pr\u00edrodovedeckej fakulte UPJ\u0160 v Ko\u0161iciach vyu\u017eil inovat\u00edvny pr\u00edstup k\u00a0v\u00fdskumu tvaru z\u0155n sediment\u00e1rnych horn\u00edn pre pochopenie transportu materi\u00e1lu v\u00a0riekach [1]. Kombin\u00e1ciou met\u00f3d skenovacieho elektr\u00f3nov\u00e9ho mikroskopu a r\u00f6ntgenovej mikrotomografie sa detailne zdokumentoval povrch z\u0155n miner\u00e1lu gran\u00e1t a poz\u00edcia inkl\u00fazi\u00ed vo vn\u00fatri z\u0155n. Tieto zobrazovacie met\u00f3dy umo\u017enili tvorbu 3D modelov povrchu z\u0155n a\u00a0jeho anal\u00fdzu. 3D anal\u00fdza povrchu je aplikovate\u013en\u00e1 v\u00a0r\u00f4znych prostrediach a\u00a0tradi\u010dne rie\u0161en\u00e1 v\u00fdskumn\u00edkmi n\u00e1\u0161ho \u00fastavu [2]. Publikovan\u00e9 v\u00fdsledky poukazuj\u00fa na zmeny, ktor\u00e9 nast\u00e1vaj\u00fa po\u010das transportu miner\u00e1lnych z\u0155n v rie\u010dnom prostred\u00ed. Tieto v\u00fdsledky maj\u00fa v\u00fdznam nielen pre pochopenie s\u00fa\u010dasn\u00fdch procesov v riekach, ale aj pre sk\u00famanie geologickej minulosti \u2013 pom\u00e1haj\u00fa rekon\u0161truova\u0165 prostredie, ak\u00e9 existovalo pred mili\u00f3nmi rokov. Z\u00e1rove\u0148 m\u00f4\u017eu by\u0165 u\u017eito\u010dn\u00e9 pri h\u013eadan\u00ed nerastn\u00fdch surov\u00edn, ke\u010f\u017ee sa podobn\u00e9 met\u00f3dy daj\u00fa vyu\u017ei\u0165 aj pri v\u00fdskume star\u0161\u00edch sedimentov [3, 4].<\/p>\n\n\n\n<p>\u0160t\u00fadia bola publikovan\u00e1 v prest\u00ed\u017enom \u010dasopise <a href=\"https:\/\/doi.org\/10.1016\/j.sedgeo.2024.106652\"><em>Sedimentary Geology<\/em><\/a> [1].<\/p>\n<\/div><\/div>\n\n\n<style>.kadence-column72044_76e35c-7d > .kt-inside-inner-col,.kadence-column72044_76e35c-7d > .kt-inside-inner-col:before{border-top-left-radius:0px;border-top-right-radius:0px;border-bottom-right-radius:0px;border-bottom-left-radius:0px;}.kadence-column72044_76e35c-7d > .kt-inside-inner-col{column-gap:var(--global-kb-gap-sm, 1rem);}.kadence-column72044_76e35c-7d > .kt-inside-inner-col{flex-direction:column;}.kadence-column72044_76e35c-7d > .kt-inside-inner-col > .aligncenter{width:100%;}.kadence-column72044_76e35c-7d > .kt-inside-inner-col:before{opacity:0.3;}.kadence-column72044_76e35c-7d{position:relative;}@media all and (max-width: 1024px){.kadence-column72044_76e35c-7d > .kt-inside-inner-col{flex-direction:column;}}@media all and (max-width: 767px){.kadence-column72044_76e35c-7d > .kt-inside-inner-col{flex-direction:column;}}<\/style>\n<div class=\"wp-block-kadence-column kadence-column72044_76e35c-7d\"><div class=\"kt-inside-inner-col\"><style>.kb-image72044_7c75c5-6f .kb-image-has-overlay:after{opacity:0.3;}<\/style>\n<div class=\"wp-block-kadence-image kb-image72044_7c75c5-6f\"><figure class=\"aligncenter size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"900\" height=\"506\" src=\"https:\/\/www.upjs.sk\/app\/uploads\/sites\/10\/2024\/09\/vms-3Dmodelovanie-092024.jpg\" alt=\"\" class=\"kb-img wp-image-72048\" srcset=\"https:\/\/www.upjs.sk\/app\/uploads\/sites\/10\/2024\/09\/vms-3Dmodelovanie-092024.jpg 900w, https:\/\/www.upjs.sk\/app\/uploads\/sites\/10\/2024\/09\/vms-3Dmodelovanie-092024-300x169.jpg 300w, https:\/\/www.upjs.sk\/app\/uploads\/sites\/10\/2024\/09\/vms-3Dmodelovanie-092024-768x432.jpg 768w\" sizes=\"(max-width: 900px) 100vw, 900px\" \/><figcaption>(1) Gran\u00e1t z rie\u010dnych sedimentov; (2) SEM obrazy gran\u00e1tu s mechanick\u00fdmi (A-C) a chemick\u00fdmi mikrotext\u00farami (D); (3) Spracovanie 3D modelov gran\u00e1tu a identifik\u00e1cia impaktov na ich povrchu.<\/figcaption><\/figure><\/div>\n<\/div><\/div>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n<style>.kadence-column72044_5337fe-2c > .kt-inside-inner-col{padding-top:var(--global-kb-spacing-xs, 1rem);padding-right:var(--global-kb-spacing-xs, 1rem);padding-left:var(--global-kb-spacing-xs, 1rem);}.kadence-column72044_5337fe-2c > .kt-inside-inner-col,.kadence-column72044_5337fe-2c > .kt-inside-inner-col:before{border-top-left-radius:5px;border-top-right-radius:5px;border-bottom-right-radius:5px;border-bottom-left-radius:5px;}.kadence-column72044_5337fe-2c > .kt-inside-inner-col{column-gap:var(--global-kb-gap-sm, 1rem);}.kadence-column72044_5337fe-2c > .kt-inside-inner-col{flex-direction:column;}.kadence-column72044_5337fe-2c > .kt-inside-inner-col > .aligncenter{width:100%;}.kadence-column72044_5337fe-2c > .kt-inside-inner-col{background-color:#F4F4F4;}.kadence-column72044_5337fe-2c > .kt-inside-inner-col:before{opacity:0.3;}.kadence-column72044_5337fe-2c{position:relative;}@media all and (max-width: 1024px){.kadence-column72044_5337fe-2c > .kt-inside-inner-col{flex-direction:column;}}@media all and (max-width: 767px){.kadence-column72044_5337fe-2c > .kt-inside-inner-col{flex-direction:column;}}<\/style>\n<div class=\"wp-block-kadence-column kadence-column72044_5337fe-2c\"><div class=\"kt-inside-inner-col\">\n<p class=\"has-text-align-justify\">[1] B\u00f3nov\u00e1, K., \u0160upinsk\u00fd, J., B\u00f3na, J., Nov\u00e1kov\u00e1, M., \u0160urka, J., Barabas, D. (2024). Changes in detrital garnet grain morphology and microtextures during fluvial transport in the Western Carpathians revealed by scanning electron microscopy and 3D model analysis: Implication for paleoenvironmental reconstruction. Sedimentary Geology, 467, 106652, 1\u201318. <a href=\"https:\/\/doi.org\/10.1016\/j.sedgeo.2024.106652\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1016\/j.sedgeo.2024.106652<\/a><\/p>\n\n\n\n<p>[2] Gallay, M., Hochmuth, Z., Ka\u0148uk, J., Hofierka, J. (2016). Geomorphometric analysis of cave ceiling channels mapped with 3D terrestrial laser scanning. Hydrolology and Earth System Sciences, 20, 1827-1849.<\/p>\n\n\n\n<p>[3] Dill, H.G., Klosa, D., Steyer, G. (2009). The \u201cDonauplatin\u201d: source rock analysis and origin of a distal fluvial Au-PGE placer in Central Europe. Miner. Petrol. 96, 141\u2013161.<\/p>\n\n\n\n<p>[4] Dill, H.G., Steyer, G., Weber, B. (2010). Morphological studies of PGM grains in alluvial-fluvial placer deposits from the Bayerischer Wald, SE Germany: Hollingworthite and ferroan platinum. Neues Jahrb. Mineral. Abh. 187, 101\u2013110.<\/p>\n<\/div><\/div>\n","protected":false},"excerpt":{"rendered":"<p>V\u00fdskumn\u00fd t\u00edm docentky Katar\u00edny B\u00f3novej z \u00dastavu geografie na Pr\u00edrodovedeckej fakulte UPJ\u0160 v Ko\u0161iciach vyu\u017eil inovat\u00edvny pr\u00edstup k v\u00fdskumu tvaru z\u0155n sediment\u00e1rnych horn\u00edn pre pochopenie transportu materi\u00e1lu v riekach<\/p>\n","protected":false},"author":25,"featured_media":72045,"template":"","meta":{"_editorskit_title_hidden":false,"_editorskit_reading_time":0,"_editorskit_is_block_options_detached":false,"_editorskit_block_options_position":"{}","footnotes":""},"categories":[],"tags":[62],"tax_aktuality":[],"class_list":["post-72044","cpt_aktuality","type-cpt_aktuality","status-publish","has-post-thumbnail","hentry","tag-uge"],"acf":{"acf_link_na_externy_obsah":"","poradie_clanku":0},"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v23.8 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Inovat\u00edvne 3D modelovanie miner\u00e1lnych z\u0155n odha\u013euje geologick\u00fa minulos\u0165 - 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