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Magnetic polarity of Upper Triassic sediments of the Germanic Basin in Poland

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Magnetic polarity of Upper Triassic sediments of the Germanic Basin in Poland

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dc.contributor.author Nawrocki, Jerzy pl
dc.contributor.author Jewuła, Karol [USOS36442] pl
dc.contributor.author Stachowska, Aleksandra pl
dc.contributor.author Szulc, Joachim [SAP11010265] pl
dc.date.accessioned 2016-01-27T10:47:58Z
dc.date.available 2016-01-27T10:47:58Z
dc.date.issued 2015 pl
dc.identifier.issn 0208-9068 pl
dc.identifier.uri http://ruj.uj.edu.pl/xmlui/handle/item/20177
dc.language eng pl
dc.rights Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa *
dc.rights.uri http://creativecommons.org/licenses/by-nc-sa/4.0/pl/legalcode *
dc.title Magnetic polarity of Upper Triassic sediments of the Germanic Basin in Poland pl
dc.type JournalArticle pl
dc.description.physical 663-674 pl
dc.description.additional Bibliogr. s. 670-674 pl
dc.abstract.en Palaeomagnetic results are presented for 205 samples of cores from the Książ Wielkopolski IG-2, Woźniki K1 and Patoka 1 wells, drilled in the Polish part of Germanic Basin. The magnetic polarity stratigraphy is based on the inclination of the characteristic remanent magnetization, isolated in 60% of the total samples and found to be in general agreement with the expected Late Triassic inclination at the sampling sites. A total of 22 magnetozones from the integration of the three records correspond to about 25% of the published polarity zones for the Upper Triassic sediments that were combined in the worldwide composite polarity-time scale. The magne- tic polarity pattern, defined for the Schilfsanstein, fits very well with the one defined in the Tethys area for the upper part of the Julian sub-stage. According to the magnetostratigraphic data, the uppermost part of the Upper Gypsum Beds (equivalent to the Ozimek Member of the redefined Grabowa Formation) and the lowermost part of the Patoka Member, containing the Krasiejów bone-breccia horizon, can be correlated with the latest Tuvalian (~228.5 Ma) or with the middle part of Lacian (~225 Ma). However, if the “Long-Tuvalian” option for the Late Triassic Time Scale is taken into consideration, the parts of these substages mentioned above should be correlated with ~221.5 Ma and ~218.5 Ma, respectively. pl
dc.subject.en magnetostratigraphy pl
dc.subject.en Grabowa Formation pl
dc.subject.en Upper Triassic pl
dc.subject.en Germanic Basin pl
dc.subject.en Poland pl
dc.description.volume 85 pl
dc.description.number 4 pl
dc.identifier.doi 10.14241/asgp.2015.026 pl
dc.identifier.eissn 2300-8512 pl
dc.title.journal Annales Societatis Geologorum Poloniae pl
dc.language.container eng pl
dc.affiliation Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych pl
dc.subtype Article pl
dc.rights.original OTHER; otwarte czasopismo; ostateczna wersja wydawcy; w momencie opublikowania; 0; pl
dc.identifier.project ROD UJ / P pl
.pointsMNiSW [2015 A]: 15


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Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa Except where otherwise noted, this item's license is described as Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa