Abstract
One of the most fundamental unresolved problems of tectonic modelling of the Archaean craton of West Greenland is the interpretation of the magmatic environment in which the ubiquitous Malene-type supracrustal rocks were formed and the relationship of these rocks to the pre-existing Amitsoq (c. 3750 m.y.) sialic crust in the Godthåbsfjord region at the centre of the craton. The Amitsoq gneisses are a complex of polyphase, pegmatite banded, tonalitic to granitic rocks and the Malene supracrustals are dominated by metavolcanic amphibolites associated with metasedimentary layers and ultrabasic bodies (Bridgwater et al., 1976). The present large scale intercalation of major Malene supracrustal and Amitsoq gneiss units is dearly the result of an early phase of thrusting (Bridgwater et al. 1974; Hall & Friend, 1979). However, whether the juxtaposition of the two suites originated from a cover-basement relationship or was purely tectonic in origin has been open to speculation.
Highlights
One of the most fundamental unresolved problems of tectonic modelling of the Archaean craton of West Greenland is the interpretation of the magmatic environment in which the ubiquitous Malene-type supracrustal rocks were formed and the relationship of these rocks to the pre-existing Amitsoq (c. 3750 m.y.) sialic crust in the Godthåbsfjord region at the centre of the craton
If the Amitsoq granitic gneisses formed an early Archaean continental crust through which the Malene metavolcanic amphibolites were originally injected to form a cover-basement relationship, numerous basic feeder dykes should be preserved within the Amitsoq gneisses
Since abundant metamorphosed basic dykes are a characteristic feature of the Amitsoq gneisses (McGregor, 1973), these rocks can obviously be postulated as feeders to the Malene metavolcanics in the Godthåbsfjord region
Summary
One of the most fundamental unresolved problems of tectonic modelling of the Archaean craton of West Greenland is the interpretation of the magmatic environment in which the ubiquitous Malene-type supracrustal rocks were formed and the relationship of these rocks to the pre-existing Amitsoq (c. 3750 m.y.) sialic crust in the Godthåbsfjord region at the centre of the craton. If the Amitsoq granitic (sensu lato) gneisses formed an early Archaean continental crust through which the Malene metavolcanic amphibolites were originally injected to form a cover-basement relationship, numerous basic feeder dykes should be preserved within the Amitsoq gneisses.
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