Far East Avalonia: its chronostratigraphic structure revealed by SHRIMP zircon ages from Upper Carboniferous to Lower Permian volcanic rocks (drill cores from Germany, Poland and Denmark).

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Far East Avalonia: its chronostratigraphic structure revealed by SHRIMP zircon ages from Upper Carboniferous to Lower Permian volcanic rocks (drill cores from Germany, Poland and Denmark).

Sensitive high-resolution ion microprobe (SHRIMP) U-Pb ages have been obtained from zircons separated from Upper Carboniferous to Lower Permian SiO2-rich volcanic and subvolcanic rocks of eleven drill sites. The volcanic rocks belong to a large volcanic province that formed during the initial stage...

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Bibliographic Details
Main Authors:	Breitkreuz, C., Kennedy, Allen, Geibler, M., Ehling, B., Kopp, J., Muszynski, A., Protas, A., Stouge, S.
Format:	Journal Article
Published:	Geological Society of America 2007
Online Access:	http://hdl.handle.net/20.500.11937/19845

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