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Published in 2018 at "Minerals"
DOI: 10.3390/min9010006
Abstract: The Paleoproterozoic (~1.8 Ga) Penokean Volcanic Belt (PVB) in the Great Lakes Region of North America hosts several polymetallic volcanogenic massive sulfide (VMS) deposits. These deposits were formed by back-arc extensional volcanism during the accretion…
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Keywords:
vms deposits;
lakes region;
volcanic belt;
great lakes ... See more keywords