The Archaean gneisses of the Nuuk area (southern West Greenland) are partitioned into tectonostratigraphic terranes - blocks of arc-like crust that evolved independently until they coalesced by collisional orogeny. To 'map' terranes to the east under th
Abstrad: The Faringehavn-Tre Bradre area consists of three distinct terranes tectonically jux-tapose...
The Archaean North Atlantic Craton of West Greenland collided at c. 1.9 Ga with a lesser-known Archa...
The Eoarchaean (>3,600 Ma) Itsaq Gneiss Complex of southern West Greenland is dominated by polyphase...
In the south of the Nuuk region of West Greenland our 1980s mapping recognized four Archaean gneiss ...
In the last three field seasons the Geological Survey of Denmark and Greenland (GEUS) has undertaken...
Geochemical methods to advance knowledge on the early Earth require supplies of well-preserved >3600...
The Mesoarchaean Kapisilik and Eoarchaean Isukasia terranes in the Nuuk region of southern West Gree...
Palaeoproterozoic and Archaean gneiss complexes in northern Greenland: Palaeoproterozoic terrane ass...
The Archean gneiss complex of West Greenland contains packages of unrelated rocks created during rel...
Constraining the source, genesis, and evolution of Archaean felsic crust is key to understanding the...
Prior to 1970 grey gneiss complexes were interpreted as partially-melted sedimentary sequences. Once...
The Precambrian shield of northern Greenland has been investigated by SHRIMP U-Pb zircon dating of 1...
The world's most extensive, well preserved, early Archaean (>3500 Ma) structures occur in the northe...
The part of the West Greenland Archean gneiss complex centered around Godthabsfjord and extending fr...
In the gneiss complex of the Nuuk region of the North Atlantic Craton in southern West Greenland, te...
Abstrad: The Faringehavn-Tre Bradre area consists of three distinct terranes tectonically jux-tapose...
The Archaean North Atlantic Craton of West Greenland collided at c. 1.9 Ga with a lesser-known Archa...
The Eoarchaean (>3,600 Ma) Itsaq Gneiss Complex of southern West Greenland is dominated by polyphase...
In the south of the Nuuk region of West Greenland our 1980s mapping recognized four Archaean gneiss ...
In the last three field seasons the Geological Survey of Denmark and Greenland (GEUS) has undertaken...
Geochemical methods to advance knowledge on the early Earth require supplies of well-preserved >3600...
The Mesoarchaean Kapisilik and Eoarchaean Isukasia terranes in the Nuuk region of southern West Gree...
Palaeoproterozoic and Archaean gneiss complexes in northern Greenland: Palaeoproterozoic terrane ass...
The Archean gneiss complex of West Greenland contains packages of unrelated rocks created during rel...
Constraining the source, genesis, and evolution of Archaean felsic crust is key to understanding the...
Prior to 1970 grey gneiss complexes were interpreted as partially-melted sedimentary sequences. Once...
The Precambrian shield of northern Greenland has been investigated by SHRIMP U-Pb zircon dating of 1...
The world's most extensive, well preserved, early Archaean (>3500 Ma) structures occur in the northe...
The part of the West Greenland Archean gneiss complex centered around Godthabsfjord and extending fr...
In the gneiss complex of the Nuuk region of the North Atlantic Craton in southern West Greenland, te...
Abstrad: The Faringehavn-Tre Bradre area consists of three distinct terranes tectonically jux-tapose...
The Archaean North Atlantic Craton of West Greenland collided at c. 1.9 Ga with a lesser-known Archa...
The Eoarchaean (>3,600 Ma) Itsaq Gneiss Complex of southern West Greenland is dominated by polyphase...