Evidence for spreading in the lower Kam Group of the Yellowknife greenstone belt: Implications for Archaean basin evolution in the Slave Province

The Yellowknife greenstone belt is the western margin of an Archean turbidite-filled basin bordered on the east by the Cameron River and Beaulieu River volcanic belts (Henderson, 1981; Lambert, 1982). This model implies that rifting was entirely ensialic and did not proceed beyond the graben stage....

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Bibliographic Details
Main Authors: Padgham, W. A., Helmstaedt, H.
Format: Other/Unknown Material
Language:unknown
Published: 1986
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Online Access:http://hdl.handle.net/2060/19860013638