https://geoscan.nrcan.gc.ca/starweb/geoscan/servlet.starweb?path=geoscan/fullf.web&search1=R=296553
Natural Resources Canada, 2015
The Ming deposit is hosted in Cambro-Ordovician intermediate to felsic rocks underlain by ca. 490 Ma ophiolite slivers of boninitic composition. The deposit...
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