Fluid-Rock Interaction Around Mafic to Intermediate Intrusions: Evidence from Trace Element and Isotopic Geochemistry of Minerals.
Collectively, this research deals with the nature of hydrothermal systems around mafic to intermediate intrusions, with implications for understanding the Sudbury structure hydrothermal system and the genesis of the Ferguson Lake Ni-Cu-Co-PGE mineralization. New isotopic and chemical data on hydroth...
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| Format: | Doctoral or Postdoctoral Thesis |
| Language: | English |
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University of Windsor
2010
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| Online Access: | https://scholar.uwindsor.ca/etd/442 https://scholar.uwindsor.ca/context/etd/article/1441/viewcontent/campos3.pdf |