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<dc:title xml:lang="en"><![CDATA[Poligeneza deformacji glacitektonicznych w utworach kenozoicznych kopalni Stanisław-Północ k. Ruska (blok przedsudecki) - wstępne wyniki badań = Polyphase glacitectonic deformations of the cenozoic deposits exposed in "Stanisław-North" opencast mine near Rusko (fore-sudetic block) - preliminary results]]></dc:title>
<dc:title xml:lang="pl"><![CDATA[Poligeneza deformacji glacitektonicznych w utworach kenozoicznych kopalni Stanisław-Północ k. Ruska (blok przedsudecki) - wstępne wyniki badań = Polyphase glacitectonic deformations of the cenozoic deposits exposed in "Stanisław-North" opencast mine near Rusko (fore-sudetic block) - preliminary results]]></dc:title>
<dc:creator><![CDATA[Hałuszczak, Andrzej]]></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[The paper describes preliminary results of structural field investigations concerning glacitectonic deformations of the Cenozoic deposits in the "Jaroszów-North" open-cast mine near Rusko village (Fore-Sudetic Block). Considering the spatial arrangement and kinematic features of studied mesostructures, it is suggested that they were related to the two separate glaciations.]]></dc:description>
<dc:description xml:lang="en"><![CDATA[The older deformations were formed during the first glaciation of the studied area ascribed to the older Elsterian stage. These structures are representing by multiple series ofimbricated thrusts that occur mainly at the open-cast floor in the Neogene clays and coaly clays. Low-angle to gently NNE dipping thrust planes exhibit sense of displacement towards the SSW.]]></dc:description>
<dc:description xml:lang="en"><![CDATA[The younger phase of glacitectonic deformations can be referred to the older Saalian Glaciation (Odranian). It is recorded by numerous thrusts, reverse faults, folds etc. (some of them override the earlier formed faults), that involve the Neogene-Quatemary deposits. Predominantly they display sense of displacement towards the SW.]]></dc:description>
<dc:description xml:lang="en"><![CDATA[Most of the mentioned above deformations are interpreted as a second-order structures related to SW-verging large thrusted fold, because of a macro-scale exposed just partly in the open cast mine. More complete reconstruction of this thrusted fold (Rusko structure) was able using a number of boreholes drilled in studied area.]]></dc:description>
<dc:description xml:lang="en"><![CDATA[Based on drill date, the Rusko structure is bounded below by the detachment surface (zone?), that lies a few meters under the open-cast tloor at a depth +150-155 m and front of this structure extends NW-SE over a distance of nearly 1 km.]]></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[The paper describes preliminary results of structural field investigations concerning glacitectonic deformations of the Cenozoic deposits in the "Jaroszów-North" open-cast mine near Rusko village (Fore-Sudetic Block). Considering the spatial arrangement and kinematic features of studied mesostructures, it is suggested that they were related to the two separate glaciations.]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[The older deformations were formed during the first glaciation of the studied area ascribed to the older Elsterian stage. These structures are representing by multiple series ofimbricated thrusts that occur mainly at the open-cast floor in the Neogene clays and coaly clays. Low-angle to gently NNE dipping thrust planes exhibit sense of displacement towards the SSW.]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[The younger phase of glacitectonic deformations can be referred to the older Saalian Glaciation (Odranian). It is recorded by numerous thrusts, reverse faults, folds etc. (some of them override the earlier formed faults), that involve the Neogene-Quatemary deposits. Predominantly they display sense of displacement towards the SW.]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[Most of the mentioned above deformations are interpreted as a second-order structures related to SW-verging large thrusted fold, because of a macro-scale exposed just partly in the open cast mine. More complete reconstruction of this thrusted fold (Rusko structure) was able using a number of boreholes drilled in studied area.]]></dc:description>
<dc:description xml:lang="pl"><![CDATA[Based on drill date, the Rusko structure is bounded below by the detachment surface (zone?), that lies a few meters under the open-cast tloor at a depth +150-155 m and front of this structure extends NW-SE over a distance of nearly 1 km.]]></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/45367/PDF/7_haluszczak_poligeneza.pdf]]></dc:identifier>
<dc:identifier><![CDATA[https://zbc.uz.zgora.pl/repozytorium/dlibra/publication/51598/edition/45367/content]]></dc:identifier>
<dc:identifier><![CDATA[oai:zbc.uz.zgora.pl:45367]]></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:51598]]></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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