Orogenic paleofluid flow recorded by discordant detrital zircons in the Caledonian foreland basin of northern Greenland

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Orogenic paleofluid flow recorded by discordant detrital zircons in the Caledonian foreland basin of northern Greenland

Concordant detrital zircon dates from Neoproterozoic to Paleozoic continental slope and trough deposits in northern Greenland indicate Late Archean and Paleoproterozoic sediment sources. Significant numbers of dates are, however, discordant and, together with a few apparently concordant dates, give...

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Bibliographic Details
Main Authors:	Morris, G., Kirkland, Chris, Pease, V.
Format:	Journal Article
Published:	Geological Society of America 2015
Online Access:	http://hdl.handle.net/20.500.11937/30926

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