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Miaskitic Rocks Ketilidian structure and the ra****vi
suite between Lindenow Fjord and Kap Farvel, South-East
Greenland The
Ketilidian orogen of South...
- The
Ketilidian orogeny was a late
Paleoproterozoic mountain-building
event that
affected southern Greenland during the
period 1.85 to 1.72 Ga. The orogenic...
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photographs of the Kap
Farvel area
Archived 2020-10-12 at the
Wayback Machine Ketilidian structure and the ra****vi
suite between Lindenow Fjord and Kap Farvel...
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concept Nena
formed c. 1,900 million
years ago in the Penokean, Makkovikan,
Ketilidian, and
Svecofennian orogenies. However,
because Nena
excludes several known...
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opened in 2004.
Nalunaq is
located 33 km
northeast of Nanortalik, in the
Ketilidian Orogenic Belt of
southern Greenland (60° 21′ 29″ N, 44° 50′ 11″ W). Gold-quartz...
- Belts, and 1.3–1.2 Ga
Elzevirian Belt in
North America; the 1.8–1.7 Ga
Ketilidian Belt in Greenland; and the 1.8–1.7
Transscandinavian Igneous Belt, 1.7–1...
-
Paleoproterozoic mountain-building
event in
Greenland – (1910–1770 Ma)
Ketilidian orogeny –
Collision at the
southern margin of the
North Atlantic Craton...
- Historic,
Cultural and
Ancient Sites sites in
Greenland New
insights on the north-eastern part of the
Ketilidian orogen in South-East
Greenland v t e...
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islands of
Islay and Colonsay. The
Rhinns complex is
correlated with the
Ketilidian metamorphic belt of
southern Greenland and the
Svecofennian of Scandinavia...
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Wayback Machine Ketilidian structure and the ra****vi
suite between Lindenow Fjord and Kap Farvel, South-East
Greenland The
Ketilidian orogen of South...
