Cretaceous-Tertiary boundary deposits in Denmark: A diachroneity-Reference-Cited by-同舟云学术

Cretaceous-Tertiary boundary deposits in Denmark: A diachroneity

Published:2004 Issue:7 Volume:69 Page:555-561
ISSN:0352-5139
Container-title:Journal of the Serbian Chemical Society
language:en
Short-container-title:JSCS

Author:

Premovic Pavle¹

Affiliation:

1. Laboratory for Geochemistry, Cosmochemistry and Astrochemistry, University of Niš, Niš, Serbia and Montenegro

Abstract

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 Kl?v/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.

Publisher

National Library of Serbia

Subject

General Chemistry

Reference15 articles.

1. Extraterrestrial Cause for the Cretaceous-Tertiary Extinction

2. Bolide impacts, acid rain, and biospheric traumas at the Cretaceous-Tertiary boundary

3. The impact of the Cretaceous/Tertiary bolide on evaporite terrane and generation of major sulfuric acid aerosol

4. Origin of microlayering in worldwide distributed Ir-rich marine Cretaceous/Tertiary boundary clays

5. Iridium, sulfur isotopes and rare earth elements in the Cretaceous-Tertiary boundary clay at Stevns Klint, Denmark

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1. Crossing the boundary: an elasmobranch fauna from Stevns Klint, Denmark;Palaeontology;2013-11-11

2. Geochemistry of the cretaceous-tertiary boundary (Fish Clay) at Stevns Klint (Denmark): Ir, Ni and Zn in kerogen;Journal of the Serbian Chemical Society;2006

3. Geochemistry of Ni in the Cretaceous-Tertiary succession Fiskeler (Fish Clay) at Stevns Klint (Denmark): cheto-smectite of the black marl;Journal of the Serbian Chemical Society;2006