Journal article
Gneiss complex of the Skaerfjorden region (76 degrees -78 degrees N), North-east Greenland
Rapport - Gronlands Geologiske Undersogelse (1964), Vol.162, pp.35-51
1994
DOI: 10.34194/rapggu.v162.8247
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
Details
- Title: Subtitle
- Gneiss complex of the Skaerfjorden region (76 degrees -78 degrees N), North-east Greenland
- Creators
- Joseph M Hull - Seattle Central Community College, Division of Science and Mathematics Seattle, WA USA United StatesJohan D FriderichsenJane A GilottiNiels HenriksenA. K HigginsFeiko Kalsbeek
- Contributors
- A. K Higgins (Editor) - Geological Survey of Greenland Copenhagen DNK Denmark
- Resource Type
- Journal article
- Publication Details
- Rapport - Gronlands Geologiske Undersogelse (1964), Vol.162, pp.35-51
- DOI
- 10.34194/rapggu.v162.8247
- ISSN
- 0418-6559
- eISSN
- 2597-2944
- Publisher
- Gronlands Geologiske Undersogelse
- Alternative title
- Geology of North-east Greenland
- Language
- English
- Date published
- 1994
- Academic Unit
- Earth and Environmental Sciences
- Record Identifier
- 9984240905202771
Metrics
8 Record Views