The nature of Ordovician limestone-marl alternations in the Oslo-Asker District (Norway): witnesses of primary glacio-eustasy or diagenetic rhythms?

Ordovician limestone-marl alternations in the Oslo-Asker District have been interpreted as signaling glacio-eustatic lowstands, which would support a prolonged “Early Palaeozoic Icehouse”. However, these rhythmites could alternatively reflect differential diagenesis, without sedimentary trigger. Her...

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Detalles Bibliográficos
Autores principales: Amberg, Chloé E. A., Collart, Tim, Salenbien, Wout, Egger, Lisa M., Munnecke, Axel, Nielsen, Arne T., Monnet, Claude, Hammer, Øyvind, Vandenbroucke, Thijs R. A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4704048/
https://www.ncbi.nlm.nih.gov/pubmed/26739251
http://dx.doi.org/10.1038/srep18787

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4704048/
https://www.ncbi.nlm.nih.gov/pubmed/26739251
http://dx.doi.org/10.1038/srep18787

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