A new age model for the Ordovician (Sandbian) K-bentonites in Oslo, Norway

Author:

Ballo Eirik G.,Augland Lars Eivind,Hammer Øyvind,Svensen Henrik H.

Funder

Norges Forskningsråd

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference72 articles.

1. On the cause of the Ordovician glaciation;Armstrong,2007

2. New U-Pb zircon ages of the Sandbian (Upper Ordovician) “Big K-bentonite” in Baltoscandia (Estonia and Sweden) by LA-ICPMS;Bauert;GFF,2014

3. Stability of the astronomical frequencies over the earth's history for paleoclimate studies;Berger;Science,1992

4. Nomenclature, stratigraphy, chemical fingerprinting, and areal distribution of some Middle Ordovician K-bentonites in Baltoscandia;Bergström;GFF,1995

5. The Upper Ordovician Guttenberg δ13C excursion (GICE) in North America and Baltoscandia: Occurrence, chronostratigraphic significance, and paleoenvironmental relationships;Bergström;Geol. Soc. Am. Spec. Pap.,2010

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