Complex 3670-3500 Ma orogenic episodes superimposed on juvenile crust accreted between 3850 and 3690 Ma, Itsaq Gneiss Complex, Southern West Greenland

The Itsaq Gneiss Complex of the Nuuk region, southern West Greenland, is dominated by 3850-3690 Ma tonalites intruded into and intercalated with lesser amounts of different ≥3850-3700 Ma supracrustal units. Published wholerock Sr and Nd isotopic studies

Bibliographic Details
Published in:The Journal of Geology
Main Authors: Friend, Clark, Nutman, Allen
Format: Article in Journal/Newspaper
Language:unknown
Published: University of Chicago Press
Subjects:
Keywords: accretion
crustal evolution
gneiss
orogeny
tonalite
Arctic
Arctic and Antarctic
Greenland
World
Antarctic
Nuuk
Antarc*
Online Access:http://hdl.handle.net/1885/80547
https://doi.org/10.1086/430239
Description
Summary:The Itsaq Gneiss Complex of the Nuuk region, southern West Greenland, is dominated by 3850-3690 Ma tonalites intruded into and intercalated with lesser amounts of different ≥3850-3700 Ma supracrustal units. Published wholerock Sr and Nd isotopic studies

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