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