High-resolution trace element chemistry across the Cretaceous-Tertiary boundary in Denmark

• Hansen, Hans Jørgen ^[1] ; Gwozdz, Raymond ^[2] ; Rasmussen, Kaare L. ^[3]
  1. [1] Geological Institute     
  2. [2] Geophysical Institute       
  3. [3] Geophysical Institute     

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• Localización: Spanish journal of palaeontology, ISSN 2255-0550, Vol. 3, Nº. 2, 1988 (Ejemplar dedicado a: REVISTA ESPAÑOLA DE PALEONTOLOGÍA), págs. 21-29
• Idioma: inglés
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  • Closely spaced samples on millimeter scale across the Cretaceous-Tertiary boundary clay in Denmark were analyzed by instrumental neutron activation analysis. The results show a strong correlation between Cr and Ir while Co, Zn, As, Sb and Au are correlated with Fe. The elemental peaks for Ir-Cr and Fe are separated by 6 mm. The Fe peak is found in burrow-fillings at the lowermost part of the boundary clay. Chromite grains extracted from boundry clay in Denmark and New Zealand show a compositional common group. The composition points to an ultrabasic (kimberlitic) origin of the chromites. Tandem accelerator mass spectroscopy demonstrated, that there are no Ir carriers in addition to elemental carbon in the boundary clay from two localities in Denmark.