The main pulse of the Siberian Traps expanded in size and composition

Emplacement of large volumes of (sub)volcanic rocks during the main pulse of the Siberian Traps occurred within <1 m.y., coinciding with the end-Permian mass extinction. Volcanics from outside the main Siberian Traps, e.g. Taimyr and West Siberia, have since long been correlated, but existing geo...

Descripción completa

Detalles Bibliográficos
Autores principales: Augland, L. E., Ryabov, V. V., Vernikovsky, V. A., Planke, S., Polozov, A. G., Callegaro, S., Jerram, D. A., Svensen, H. H.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6904769/
https://www.ncbi.nlm.nih.gov/pubmed/31822688
http://dx.doi.org/10.1038/s41598-019-54023-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6904769/
https://www.ncbi.nlm.nih.gov/pubmed/31822688
http://dx.doi.org/10.1038/s41598-019-54023-2

Ejemplares similares