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...
| Main Authors: | , , |
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| Format: | Journal Article |
| Published: |
Geological Society of America
2015
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| Online Access: | http://hdl.handle.net/20.500.11937/30926 |