Palaeoproterozoic age of a basement gneiss complex in the Charcot Land tectonic window, East Greenland Caledonides

The Charcot Land tectonic window exposes crystalline basement gneisses, which form part of the foreland of the East Greenland Caledonides. These gneisses were previously believed to be Archaean in age, on the basis of imprecise K-Ar analyses carried out in the early 1980s on hornblende from amphibol...

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Bibliographic Details
Published in:Geological Survey of Denmark and Greenland (GEUS) Bulletin
Main Author: Thrane, Kristine
Format: Article in Journal/Newspaper
Language:English
Published: Geological Survey of Denmark and Greenland (GEUS) 2004
Subjects:
Caledonides
East Greenland
geochronology
Palaeoproterozoic
Greenland
Charcot
Charcot Land
Online Access:https://geusbulletin.org/index.php/geusb/article/view/4818
https://doi.org/10.34194/geusb.v6.4818

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