Please use this identifier to cite or link to this item: https://hdl.handle.net/10593/10807
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dc.contributor.authorIssmer, Katarzyna-
dc.date.accessioned2014-05-21T08:33:53Z-
dc.date.available2014-05-21T08:33:53Z-
dc.date.issued2010-
dc.identifier.citationBadania Fizjograficzne, Seria A, Tom 61, 2010, s. 169-180pl_PL
dc.identifier.isbn978-83-7654-010-8-
dc.identifier.issn2081-6014-
dc.identifier.urihttp://hdl.handle.net/10593/10807-
dc.description.abstractMagnetic susceptiblity (Ms) gives precise information about paleo-environmetal changes. The statistical relation between Ms and precise grain-size analysis of loess from Dalków Hills implies that any interpretation of the paleoclimatic record of loess sequences must recognize the detailed grain-size, because such relation could well imply paleo-environmetal changes in sediments without organic residuum. The data presented here suggest that environmental magnetic analysis of loess sediments is mainly dependent on fine silt content described in Aeolian literature as loess fraction. This study indicates that multiple methods should be employed in analyzing paleoclimatic changes recorded by magnetic susceptibility (Ms) in the Polish loess-paleosol sequences. Magnetic susceptibility (Ms) correlated with precise paleoclimatic grain-size investigations has yielded numerous records and resources.pl_PL
dc.language.isoplpl_PL
dc.publisherWydawnictwo Poznańskiego Towarzystwa Przyjaciół Naukpl_PL
dc.relation.ispartofseriesSeria A Geografia Fizyczna R.I (A61);-
dc.subjectWzgórza Dalkowskiepl_PL
dc.subjectLoessespl_PL
dc.subjectmagnetic susceptibilitypl_PL
dc.titleWpływ cech litologicznych na podatność magnetyczną lessów z rejonu Wzgórz Dalkowskichpl_PL
dc.typeArtykułpl_PL
dc.description.tomeA61pl_PL
dc.description.pageof169pl_PL
dc.description.pageto180pl_PL
Appears in Collections:Badania Fizjograficzne, Seria A, Tom 61, 2010

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