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Statements

Subject Item
dbr:North_Atlantic_Craton
dbo:wikiPageWikiLink
dbr:Ketilidian_orogeny
Subject Item
dbr:Geology_of_Greenland
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dbr:Ketilidian_orogeny
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dbr:Nena_(supercontinent)
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dbr:Ketilidian_orogeny
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rdfs:label
Ketilidian orogeny
rdfs:comment
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 belt formed during this event, sometimes known as the Ketilidian mobile belt, forms the southern boundary to the mainly Archaean North Atlantic Craton. The belt is 250–350 km wide, much of it covered by ice. It is correlated with the Makkovik Province in Labrador, Canada, which has a similar history.
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dbc:Geology_of_Greenland dbc:Proterozoic_North_America dbc:Paleoproterozoic_orogenies dbc:Orogenies_of_North_America
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1063791437
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dbc:Orogenies_of_North_America dbr:Orogeny dbr:Paleoproterozoic dbr:Year dbc:Paleoproterozoic_orogenies dbc:Proterozoic_North_America dbr:Greenland dbr:Labrador dbc:Geology_of_Greenland dbr:North_Atlantic_Craton
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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 belt formed during this event, sometimes known as the Ketilidian mobile belt, forms the southern boundary to the mainly Archaean North Atlantic Craton. The belt is 250–350 km wide, much of it covered by ice. It is correlated with the Makkovik Province in Labrador, Canada, which has a similar history.
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wikipedia-en:Ketilidian_orogeny?oldid=1063791437&ns=0
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wikipedia-en:Ketilidian_orogeny
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dbr:Ketilidian_mobile_belt
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