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Świąder, Andrzej

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inżynieria środowiska, górnictwo i energetyka
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ORCID: 0000-0003-1641-7962 
Web of Science: D-1220-2013 
ScopusID: 57215607310 
PBN - Polish Scientific Bibliography 
OPI - Polish Science Database 
Systemy AGH
Bibliografia: BaDAP AGH 
SkOs AGH 
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Now showing 1 - 4 of 4
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Compositional differences between Besko and Otryt sandstones of the Krosno Beds (Oligocene) in Eastern part of the Silesian Tectonic Unit
    (Wydawnictwa AGH, 2016) Godlewski, Paweł; Wendorff, Marek; Świąder, Andrzej
    The Krosno Formation (Oligocene) in the Silesian Tectonic Unit of the E part of the Polish Outer Carpathians is represented by two lithofacies called the Besko (or Lesko) and the Otryt facies.
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Implementation of digital maps and documentation of the site based on geographic information system for the selected regions of oil trail abstract
    (Wydawnictwa AGH, 2014) Góra, Adrianna; Franczak, Szymon; Lupa, Michał; Solecki, Marek; Cygal, Adam; Świąder, Andrzej
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    A conception of a mountain geopark in a SPA region; example of a projected Geopark »Wisłok Valley - The Polish Texas«, in the Krosno region
    (Wydawnictwa AGH, 2016) Wasiluk, Radosław; Radwanek-Bąk, Barbara; Bąk, Bogusław; Kopciowski, Robert; Malata, Tomasz; Kochman, Alicja; Świąder, Andrzej
    The Polish Geological Institute – National Research Institute (PGI – NRI), in cooperation with AGH University of Science and Technology in Krakow carried out the project of new geopark in Poland – »Wisłok Valley – The Polish Texas«. It is located in the Polish Outer Carpathians (SE part of Poland). Oil fields, mineral water, nappe tectonics and other geological components of the Outer Carpathians constitute important elements of the geodiversity of this region. The area is located in the Krosno neighbourhood and encloses a zone of about 1000 km$^{2}$. The Iwonicz-Zdrój – Rymanów-Zdrój SPA region is also included in the research area. It covers 20 municipalities of the Podkarpackie province. For the project of the Geopark, a geotouristic map, geosites, geological-educational paths, website, advertising brochures, geological-educational tables and a movie were made, which promote geotourism. The final product will be targeted at regional and local public administration bodies, national and landscape Parks, the State Forests National Forest Holding and local tourist organizations.
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Lithostratigraphic classification of the Tsodilo Hills Group: a Palaeo- to Mesoproterozoic metasedimentary succession in NW Botswana
    (Wydawnictwa AGH, 2019) Wendorff, Marek; Świąder, Andrzej
    The Tsodilo Hills Group strata exposed in the Tsodilo Hills are an association of meta-arenites, metaconglomerates, quartz-mica schists, sandstone, red siltstone and sedimentary breccia deposited on an open siliciclastic marine shelf between the Late Palaeoproterozic and Late Mesoproterozoic, and outcropping in NW Botswana. The succession is dominated by three micaceous quartzite units interlayered with subordinate lenses and wedges of other rock types. Facies gradients from S to N are expressed by: decreasing content of muscovite at all levels of metasediment organisation from thin wedge-shaped units to thick quartzite complexes, as well as a decrease in pebble content and increase in arenaceous matrix in some metaconglomerate beds, matching regional palaeotransport direction. Well-rounded pebbles of extrabasinal rocks are flat, suggesting redeposition from a beach environment. Lenticular conglomeratic bodies with erosional lower boundaries represent infills of local incisions in the sandy bottom sediments. The abundance of laterally discontinuous lithological units reflects shelf palaeotopography controlled and modified by deposition and migration of large bed forms, ranging from megaripple marks (or submarine dunes) to sand waves. Deposition was influenced by tides and two regressive events. The older regression resulted in a marker unit of tidal mudflat-related red-bed facies: mudstone, siltstone, channel-fill sandstone and sedimentary breccia. The second regression is indicated by a tabular conglomerate marker reflecting increased input of coarse terrigenous material.