{"id":43511,"date":"2019-02-06T03:21:43","date_gmt":"2019-02-06T03:21:43","guid":{"rendered":"https:\/\/www.upjs.sk\/prirodovedecka-fakulta\/20217-2\/"},"modified":"2022-11-10T20:24:07","modified_gmt":"2022-11-10T20:24:07","slug":"20217-2","status":"publish","type":"page","link":"https:\/\/www.upjs.sk\/prirodovedecka-fakulta\/en\/research\/20217-2\/","title":{"rendered":"Institute of Geography"},"content":{"rendered":"<p>Flysch Belt represents a characteristic arc along the outer periphery of the Western Carpathians. It consists of sedimentary rocks deposited during the Mesozoic to Tertiary period in the deep-sea sedimentary basins, such as the Magura basin. The source areas, which supplied the sedimentary material, as thick as several kilometres, are still intensively discussed. Eocene (Tertiary) Makovica sandstones of the Magura Nappe were studied by researchers of the Institute of Geography, in collaboration with the Earth Science Institute of the Slovak Academy of Sciences, the Geological Institute of Dion\u00fdz \u0160t\u00far and the Polish Geological Institute. They published the findings in the established journal of Palaeogeography, Palaeoclimatology, Palaeoecology. The unique aspect of the research is in the first U-Pb radiometric dating obtained from the detrital zircons indicates the Proterozoic to Variscan age (~ 2200\u2013260 million years) of their parent rocks. Heavy-mineral analysis coupled with the palaeocurrent measurements (textural features on the surface of sedimentary rock layers occurred during the sedimentation) and the acquired age data locate the source regions outside the Carpathian domain, presumably in the \u200b\u200bTisia microcontinent and Marmarosh massif, which are currently situated in the territory of Southern Hungary, Romania and Transcarpathian Ukraine.<\/p>\n<p> <a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0031018218304383\" target=\"_blank\" rel=\"noopener\">https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0031018218304383<\/a><\/p>\n<p><img decoding=\"async\" src=\"https:\/\/www.upjs.sk\/images\/fullsize\/20197\/v_4\/\" style=\"height:653px; width:800px\" \/><img decoding=\"async\" src=\"https:\/\/www.upjs.sk\/images\/fullsize\/20197\/v_5\/\" style=\"height:651px; width:800px\" \/><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Flysch Belt represents a characteristic arc along the outer periphery of the Western Carpathians. It consists of sedimentary rocks deposited during the Mesozoic to Tertiary period in the deep-sea sedimentary basins, such as the Magura basin. The source areas, which supplied the sedimentary material, as thick as several kilometres, are still intensively discussed. Eocene (Tertiary) &hellip; <a href=\"https:\/\/www.upjs.sk\/prirodovedecka-fakulta\/en\/research\/20217-2\/\">Continued<\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":43927,"menu_order":26,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_editorskit_title_hidden":false,"_editorskit_reading_time":0,"_editorskit_is_block_options_detached":false,"_editorskit_block_options_position":"{}","footnotes":""},"class_list":["post-43511","page","type-page","status-publish","hentry"],"acf":{"acf_link_na_externy_obsah":""},"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v23.9 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Institute of Geography - Pr\u00edrodovedeck\u00e1 fakulta | UPJ\u0160<\/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:\/\/www.upjs.sk\/prirodovedecka-fakulta\/en\/research\/20217-2\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Institute of Geography - Pr\u00edrodovedeck\u00e1 fakulta | UPJ\u0160\" \/>\n<meta property=\"og:description\" content=\"Flysch Belt represents a characteristic arc along the outer periphery of the Western Carpathians. It consists of sedimentary rocks deposited during the Mesozoic to Tertiary period in the deep-sea sedimentary basins, such as the Magura basin. The source areas, which supplied the sedimentary material, as thick as several kilometres, are still intensively discussed. 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