There are some superb examples on the Nuussuaq peninsula in central West Greenland - the Tartunaq intrusions. The Nuussuaq Basin is bounded on its east by a large normal fault with a throw > 1.5 km. It is intruded by a large dyke. There are other intrusions nearby, mostof which seem to be controlled by structure. Not much published about them, but they are shown on the geological map: See http://www.geus.dk/program-areas/raw-materials-greenl-map/greenland/gr-map/sh_03b.jpg
The area is readily accessible in the summer.
If you need any more info, let me know.
Jim Chalmers
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