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dc.contributor.authorKrzywiec, Piotr-
dc.contributor.authorGągała, Łukasz-
dc.contributor.authorMazur, Stanisław-
dc.contributor.authorKufrasa, Mateusz-
dc.contributor.authorŻaba, Jerzy-
dc.contributor.authorGaidzik, Krzysztof-
dc.date.accessioned2020-05-05T12:37:21Z-
dc.date.available2020-05-05T12:37:21Z-
dc.date.issued2018-
dc.identifier.citationGeophysical Research Abstracts, Vol. 20 (2018), s. 10130pl_PL
dc.identifier.issn1029-7006-
dc.identifier.issn1607-7962-
dc.identifier.urihttp://hdl.handle.net/20.500.12128/13832-
dc.description20th EGU General Assembly, EGU2018, Proceedings from the conference held 4-13 April, 2018 in Vienna, Austriapl_PL
dc.description.abstractRecent years have brought a significant progress in understanding of the external Variscides in Poland. Combined POLCRUST-01 and PolandSPAN deep seismic surveys imaged for the first time a Variscan thin-skinned fold-and-thrust belt that encroaches onto a little deformed basement slope of the East European Craton (EEC) much farther eastward than the previously postulated position of the Variscan deformation front. This deformed belt consists of several tectonic units, to a various degree overprinted by Variscan shortening and inversion (Fragment tekstu).pl_PL
dc.language.isoenpl_PL
dc.rightsUznanie autorstwa 3.0 Polska*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/pl/*
dc.subjectseismic reflectionpl_PL
dc.subjectproceedings from the conferencepl_PL
dc.subjectSE Polandpl_PL
dc.subjectEast European Cratonpl_PL
dc.titleDeep seismic reflection profiles in SE Poland reveal a Variscan thin-skinned fold-and-thrust belt encroaching the East European Cratonpl_PL
dc.typeinfo:eu-repo/semantics/conferenceProceedingspl_PL
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Uznanie Autorstwa 3.0 Polska Creative Commons Creative Commons