The onset of flood volcanism in the north-western part of the Siberian Traps: Explosive volcanism versus effusive lava flows

The Siberian Traps large igneous province was formed during the end-Permian, about 252Ma ago. Basaltic melt was injected into the organic and salt rich Tunguska sedimentary basin, forming interconnected sill complexes and associated hydrothermal vent complexes. Thick deposits of basaltic tuff and te...

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Veröffentlicht in:	Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2016-01, Vol.441, p.38-50
Hauptverfasser:	Jerram, Dougal A., Svensen, Henrik H., Planke, Sverre, Polozov, Alexander G., Torsvik, Trond H.
Format:	Artikel
Sprache:	eng
Schlagworte:	Extinction Flood basalt Freshwater Large igneous province Siberia Tuff
Online-Zugang:	Volltext
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