Evolution and emplacement of Archaean terranes in the Kapisigdlit area, southern West Greenland
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In the Godthåbsfjord region, early Archaean Arnitsoq gneisses are found in association with the middle Archaean Nûk gneisses (McGregor, 1973). Early models of crustal evolution in the Godthåbsfjord region suggested that the Amitsoq gneisses were reworked in a major crustal accretion-differentiation event, which was marked by the injection of the voluminous Nûk gneisses (e.g. Bridgwater et al., 1974; McGregor, 1979; Moor- - bath et al., 1986). This event ,has been interpreted as having culminated in a granulite-amphibolite facies metamorphic event at c. 2800 Ma, which outlasted all significant ductile deformation (e.g. Wells, 1979; Coe, 1980).
2003 ◽
Vol 75
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pp. 109-128
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2007 ◽
Vol 79
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pp. 441-455
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2006 ◽
Vol 11
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pp. 145-162
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2007 ◽
Vol 153
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pp. 29-45
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1986 ◽
Vol 50
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pp. 217-221
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1975 ◽
Vol 12
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pp. 158-173
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1994 ◽
Vol 31
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pp. 583-596
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