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The genesis of the carbon dioxide in the Polish Outer Carpathians : Szczawa tectonic window case study : new insight

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The genesis of the carbon dioxide in the Polish Outer Carpathians : Szczawa tectonic window case study : new insight

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dc.contributor.author Oszczypko, Nestor [SAP11011866] pl
dc.contributor.author Wójcik-Tabol, Patrycja [SAP11018118] pl
dc.contributor.author Oszczypko-Clowes, Marta [SAP11017382] pl
dc.date.accessioned 2018-12-18T14:47:53Z
dc.date.available 2018-12-18T14:47:53Z
dc.date.issued 2018 pl
dc.identifier.issn 0001-5709 pl
dc.identifier.uri https://ruj.uj.edu.pl/xmlui/handle/item/64230
dc.language eng pl
dc.rights Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 3.0 Polska *
dc.rights.uri http://creativecommons.org/licenses/by-nc-nd/3.0/pl/legalcode *
dc.title The genesis of the carbon dioxide in the Polish Outer Carpathians : Szczawa tectonic window case study : new insight pl
dc.type JournalArticle pl
dc.description.physical 181-206 pl
dc.description.additional Bibliogr. s. 202-206 pl
dc.identifier.weblink http://journals.pan.pl/dlibra/publication/124815/edition/108889/content pl
dc.identifier.weblink https://geojournals.pgi.gov.pl/agp/article/view/26018 pl
dc.abstract.en In the Polish sector of the Magura Nappe have long been known and exploited carbonate mineral waters, saturated with carbon dioxide, known as the "shchava (szczawa)". These waters occur mainly in the Krynica Subunit of the Magura Nappe, between the Dunajec and Poprad rivers, close to the Pieniny Klippen Belt (PKB). The origin of these waters is still not clear, this applies to both "volcanic" and "metamorphic" hypotheses. Bearing in mind the case found in the Szczawa tectonic window and our geological and geochemical studies we suggest that the origin of the carbon dioxide may be linked with the thermal/pressure alteration of organic matter of the Oligocene deposits from the Grybów Unit. These deposits, exposed in several tectonic windows of the Magura Nappe, are characterized by the presence of highly matured organic matter - the origin of the hydrocarbon accumulations. This is supported by the present-day state of organic geochemistry studies of the Carpathian oil and gas bed rocks. In our opinion origin of the carbon-dioxide was related to the southern, deep buried periphery of the Carpathian Oil and Gas Province. The present day distribution of the carbonated mineral water springs has been related to the post-orogenic uplift and erosion of the Outer (flysch) Carpathians. pl
dc.subject.en Outer Carpathians pl
dc.subject.en Grybów Unit pl
dc.subject.en Szczawa tectonic window pl
dc.subject.en mineralogy pl
dc.subject.en geochemistry pl
dc.subject.en organic matter pl
dc.subject.en carbonate mineral waters pl
dc.subject.en Carbon dioxide pl
dc.description.volume 68 pl
dc.description.number 2 pl
dc.identifier.doi 10.1515/agp-2018-0001 pl
dc.identifier.eissn 2300-1887 pl
dc.title.journal Acta Geologica Polonica pl
dc.language.container eng pl
dc.date.accession 2020-12-04 pl
dc.affiliation Wydział Geografii i Geologii : Instytut Nauk Geologicznych pl
dc.subtype Article pl
dc.rights.original CC-BY-NC-ND; otwarte czasopismo; ostateczna wersja wydawcy; w momencie opublikowania; 0 pl
dc.identifier.project ROD UJ / OP pl
.pointsMNiSW [2018 A]: 25


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Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 3.0 Polska Except where otherwise noted, this item's license is described as Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 3.0 Polska