Vein geometry and hydrostatics during Yellowknife mineralisation

Three vein systems with distinct geometry and time relations are located within major ductile shear zones at Yellowknife. En échelon arrays of centimetre width quartz veins initiated at ~45° to the shear zone boundaries and normal to the schistosity during initial translation on the structures. Thes...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Kerrich, R., Allison, I.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1978
Subjects:
Online Access:http://dx.doi.org/10.1139/e78-169
http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-169