Journal of the Serbian Chemical Society 2004 Volume 69, Issue 7, Pages: 555-561
https://doi.org/10.2298/JSC0407555P
Full text (
164 KB)
Cited by
Cretaceous-Tertiary boundary deposits in Denmark: A diachroneity
Premović Pavle I. (Laboratory for Geochemistry, Cosmochemistry and Astrochemistry, University of Niš, Niš, Serbia and Montenegro)
The lateral distribution of predominantly terrestrial kerogen or humics enriched with copper(II) porphyrins (Cu-P) across the Danish marine basin implies that the alleged Cretaceous-Tertiary (KT) boundary deposits in western Denmark (at the Nye Kløv/Dania locations)were probably formed by erosion/emplacement of the boundary clay (Fiskeler) in eastern Denmark by marine currents, as originally proposed by Hulteberg.1,2.
Keywords: diachroneity, kerogen, copper(II) porphyrins, Cretaceous-Tertiary, Fiskeler, boundary clay