Colombian-style emerald mineralization in the northern Canadian Cordillera: integration into a regional Paleozoic fluid flow regime

Emerald in the Mackenzie Mountains is hosted in extensional quartz–carbonate veins cutting organic-poor Neoproterozoic sandstones and siltstones within the hanging wall of a thrust fault that emplaced these strata above Paleozoic rocks. Isotopic compositions of water extracted from emerald are typic...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Hewton, M.L., Marshall, D.D., Ootes, L., Loughrey, L.E., Creaser, R.A.
Other Authors: Hanley, Jacob
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2013
Subjects:
Dee
Online Access:http://dx.doi.org/10.1139/cjes-2012-0128
http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2012-0128
http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2012-0128