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Gneiss complex of the Skaerfjorden region (76 degrees -78 degrees N), North-east Greenland
Journal article   Open access

Gneiss complex of the Skaerfjorden region (76 degrees -78 degrees N), North-east Greenland

Joseph M Hull, Johan D Friderichsen, Jane A Gilotti, Niels Henriksen, A. K Higgins and Feiko Kalsbeek
Rapport - Gronlands Geologiske Undersogelse (1964), Vol.162, pp.35-51
1994
DOI: 10.34194/rapggu.v162.8247
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https://doi.org/10.34194/rapggu.v162.8247View
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Abstract

The crystalline rocks of the Skærfjorden region are dominated by grey migmatitic orthogneisses with smaller bodies of ultramafic, mafic and metasedimentary lithologies. Archaean rocks (c. 3.0 Ga) have been documented, but crustal additions were predominantly Early Proterozoic (2.0–1.75 Ga) in age, reflecting subduction zone magmatism. FolIowing Early Proterozoic orogenesis and migmatisation, granitic sheets (c. 1.7 Ga) and dolerite dykes were intruded. These intrusive rocks were subsequently deformed and metamorphosed in the Caledonian orogeny (c. 400 Ma). The Skærfjorden region is located in the Caledonian hinterland, where orogen parallel stretching and extension followed an early nappe stage
Greenland Structural Geology Trace Elements Archean Arctic region Caledonian Orogeny crystalline rocks deformation dikes East Greenland fabric folds gneisses Igneous and metamorphic petrology intrusions major elements metamorphic rocks metamorphism metasedimentary rocks migmatization nappes Northern Greenland orthogneiss Paleozoic Precambrian Skaerfjorden

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