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<dc:title xml:lang="en"><![CDATA[Zjawiska glacitektoniczne w kopalni Bełchatów (2003-2005) = Glaciotectonic fenomena in Bełchatow mine (open pit) (2003-2005)]]></dc:title>
<dc:title xml:lang="pl"><![CDATA[Zjawiska glacitektoniczne w kopalni Bełchatów (2003-2005) = Glaciotectonic fenomena in Bełchatow mine (open pit) (2003-2005)]]></dc:title>
<dc:creator><![CDATA[Bruj, Małgorzata]]></dc:creator>
<dc:creator><![CDATA[Krysiak, Zofia]]></dc:creator>
<dc:subject xml:lang="en"><![CDATA[X jubileuszowe sympozjum glacitektoniki]]></dc:subject>
<dc:subject xml:lang="pl"><![CDATA[X jubileuszowe sympozjum glacitektoniki]]></dc:subject>
<dc:description xml:lang="en"><![CDATA[Glaciotectonic structures in Pleistocene deposits of Bełchatow Mine have been studied since 2003 to 2005y. Four Western (highest) walls of cover were mapped and the part of the Northern wall too (fig. l). Numerous glaciotectonic structures, sediment flows or liquefaction and neotectonic features were noticed.]]></dc:description>
<dc:description xml:lang="en"><![CDATA[Complicated deformations are visible mainly in sandygravel sediments and muds between two till horizons, however the tills are also locally deformed. The following deformational structures were distinguished: diapirs, loadings, complementary shears, different fold types, slices, detachments, duplexes, cylindrical shears, normai and reverse faults. Ifs very difficult to state which of the structures have glaciotectonic origin, which one reflect basement tectonics and which of them have neotectonic origin.]]></dc:description>
<dc:description xml:lang="en"><![CDATA[The same difficulties relate to attempt of age definition. Essentiul controlling factor of small glaciotectonic structures is pore water pressure. The other important parameters are: sediment granulometry, its content and/or character, basement configuration and Glacier-ice speed. Results of mesostructural analysis indicate a sub-horizontal direction of compression. It changes from NNE-SSW and N-S in the bottom of the profile, through NW-SE in the middle part to W-E in the top.]]></dc:description>
<dc:description xml:lang="en"><![CDATA[Changes of stress field during the time, reflect 2 deformational stages: compression (N-S) = reaction of the main structures of Bełchatow Graben to the Glacier pressure (which had left The Lower till). Compression NW-SE and W-E correspond with Glacier movement direction (which had left the Upper till) - so called Widawka lobe.]]></dc:description>
<dc:description xml:lang="en"><![CDATA[nr 5-11 tytuł: Politechnika Zielonogórska - Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="en"><![CDATA[nr 1-4 tytuł: Wyższa Szkoła Inżynierska im. Jurija Gagarina w Zielonej Górze - Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="en"><![CDATA[seria główna: Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="en"><![CDATA[zeszyt 14 ukazał się jako nr 134 serii głównej]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[Glaciotectonic structures in Pleistocene deposits of Bełchatow Mine have been studied since 2003 to 2005y. Four Western (highest) walls of cover were mapped and the part of the Northern wall too (fig. l). Numerous glaciotectonic structures, sediment flows or liquefaction and neotectonic features were noticed.]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[Complicated deformations are visible mainly in sandygravel sediments and muds between two till horizons, however the tills are also locally deformed. The following deformational structures were distinguished: diapirs, loadings, complementary shears, different fold types, slices, detachments, duplexes, cylindrical shears, normai and reverse faults. Ifs very difficult to state which of the structures have glaciotectonic origin, which one reflect basement tectonics and which of them have neotectonic origin.]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[The same difficulties relate to attempt of age definition. Essentiul controlling factor of small glaciotectonic structures is pore water pressure. The other important parameters are: sediment granulometry, its content and/or character, basement configuration and Glacier-ice speed. Results of mesostructural analysis indicate a sub-horizontal direction of compression. It changes from NNE-SSW and N-S in the bottom of the profile, through NW-SE in the middle part to W-E in the top.]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[Changes of stress field during the time, reflect 2 deformational stages: compression (N-S) = reaction of the main structures of Bełchatow Graben to the Glacier pressure (which had left The Lower till). Compression NW-SE and W-E correspond with Glacier movement direction (which had left the Upper till) - so called Widawka lobe.]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[nr 5-11 tytuł: Politechnika Zielonogórska - Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[nr 1-4 tytuł: Wyższa Szkoła Inżynierska im. Jurija Gagarina w Zielonej Górze - Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[seria główna: Zeszyty Naukowe]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[zeszyt 14 ukazał się jako nr 134 serii głównej]]></dc:description>
<dc:publisher><![CDATA[Zielona Góra: Oficyna Wydawnicza Uniwersytetu Zielonogórskiego]]></dc:publisher>
<dc:contributor><![CDATA[Gontaszewska-Piekarz, Agnieszka - red.]]></dc:contributor>
<dc:date><![CDATA[2007]]></dc:date>
<dc:type xml:lang="en"><![CDATA[artykuł]]></dc:type>
<dc:type xml:lang="pl"><![CDATA[artykuł]]></dc:type>
<dc:format xml:lang="en"><![CDATA[application/pdf]]></dc:format>
<dc:format xml:lang="pl"><![CDATA[application/pdf]]></dc:format>
<dc:identifier><![CDATA[http://www.zbc.uz.zgora.pl/repozytorium/Content/45361/PDF/1_bruj_zjawiska.pdf]]></dc:identifier>
<dc:identifier><![CDATA[https://zbc.uz.zgora.pl/repozytorium/dlibra/publication/51592/edition/45361/content]]></dc:identifier>
<dc:identifier><![CDATA[oai:zbc.uz.zgora.pl:45361]]></dc:identifier>
<dc:source xml:lang="en"><![CDATA[Zeszyty Naukowe Uniwersytetu Zielonogórskiego, Tom 14]]></dc:source>
<dc:source xml:lang="pl"><![CDATA[Zeszyty Naukowe Uniwersytetu Zielonogórskiego, Tom 14]]></dc:source>
<dc:language><![CDATA[pol]]></dc:language>
<dc:language><![CDATA[eng]]></dc:language>
<dc:relation><![CDATA[oai:zbc.uz.zgora.pl:publication:51592]]></dc:relation>
<dc:rights xml:lang="en"><![CDATA[Biblioteka Uniwersytetu Zielonogórskiego]]></dc:rights>
<dc:rights xml:lang="pl"><![CDATA[Biblioteka Uniwersytetu Zielonogórskiego]]></dc:rights>
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