The geology and geochemistry of gold mineralization in the Betts Big Pond area, Newfoundland.
The ultramafic member of the Lower Ordovician Betts Cove Ophiolite Complex forms an elongate fault bounded belt on the eastern side of the Baie Verte Peninsula. The Betts Big Pond area encompasses the transition between the least altered layered cumulate rocks of the southern part of the ultramafic...
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University of Ottawa (Canada)
2009
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| Online Access: | http://hdl.handle.net/10393/6465 http://dx.doi.org/10.20381/ruor-11289 |