Nagssugtoqidian orogeny
The Nagssugtoqidian orogeny was a late
subduction zones within the belt, have enabled its interpretation in terms of plate tectonics.[2]
References
- ^ Mayborn, K.R.; Lesher, C.E. (2006). "Origin and evolution of the Kangâmiut mafic dyke swarm, West Greenland" (PDF). In Garde, A.A.; Kalsbeek, F. (eds.). Precambrian crustal evolution and Cretaceous-Palaeogene faulting in West Greenland. Geological Survey of Denmark and Greenland Bulletin. Vol. 11. pp. 61–86.
- ISBN 9781862393035.