Upper Ordovician to Silurian facies patterns in eastern Ellesmere Island and western North Greenland and their bearing on the Nares Strait lineament
The upper Ordovician and lower Silurian sediments in the northern Nares Strait region formed during a series of platform margin collapses and platform subsidences. Facies changes from platform carbonates to slope and trough elastics are intricate, but two almost vertical facies fronts can be correla...
Published in: | Meddelelser om Grønland. Geoscience |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
The Commission for Scientific Research in Greenland /Danish Polar Center
1982
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Subjects: | |
Online Access: | https://tidsskrift.dk/meddrgroenland_geosci/article/view/139575 |