Greenland geological environments favourable for mining

H. Stendal, B.M. Stensgaard, K. Secher

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Resumé

The Greenland shield was created during the Archaean era by the amalgamation of oceanic and new arc-formed crust, followed by emplacement of granitic plutons. This was succeeded by orogenic deformation and greenschist to granulite facies metamorphism. From the Palaeoproterozoic era, orogenic activity and rifting evolution have resulted in strong possibilities for the existence of viable economic occurrences.
OriginalsprogEngelsk
UdgivelsesstedCopenhagen
ForlagGEUS
Antal sider2
DOI
StatusUdgivet - feb. 2009

Publikationsserier

NavnExploration and mining in Greenland Fact Sheet
Nummer22
ISSN1602-8171

Emneord

  • Greenland

Programområde

  • Programområde 4: Mineralske råstoffer

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