Aeromag 1996 |
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Description of an aeromagnetic survey in Greenland 1996 |
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| The Aeromag 1996 project covered a large part of South-West Greenland.
The main geological units in the survey area are the Archean craton to the north and the Palaeoproterozoic Ketilidian orogen to the south, where most of the survey area lies within in the Archean craton. The Archean craton of Greenland is the largest and best exposed craton of the North Atlantic cratons. It consists mainly of granitoid quatzo-feldspathic gneisses probably largely derived from acid to intermediate igneous rocks, but encompasses also rafts of amphibolites. There are many occurrences of supracrustal rocks of varying age within the surveyed area, however, the Tartoq group in the southern part of the Aeromag 1996 project area is the best known of the supracraustal sequences. Most of the craton experienced serveral phases of folding, faulting and/or metamorphism, often in granulite facies. The Fiskenæsset complex is situated within the Aeromag 1996 project area, near its northern boundary. It is a stratiform intrusion covering an area of approximately 2500 km2 containing anorthosites, leucogabbro and gabbro with minor amounts of ultramafic rocks and chromite. The Fiskenæsset complex and has been dated to approximately 2800 Ma. In the southern part of the Aeromag 1996 project area the Archean gneisses are at places unconformably overlain by well preserved undeformed and unmetamorphosed Palaeoproterozoic sediments and basic volcanic rocks. Further to the south these sediments become strongly deformed and metamorphosed by the Palaeoproterozoic Ketilidian orogenic belt. This is the 'Border Zone' between the Archaean craton and the Palaeoproterozoic Ketilidian orogen. See also Aeromag 1995. |
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Last modified: - © Geological Survey of Denmark and Greenland (GEUS)