Zircon alteration in wallrock of Pamour and Hoyle Pond Au deposits, Abitibi granite-greenstone belt: Constraints on timescales of fluid flow from depth-profiling techniques
Quartz-carbonate vein Au deposits in the Timmins-Porcupine gold camp, Abitibi Subprovince, have equivocal protracted parageneses and formed during late to post-Kenoran (2750-2670 Ma) deformation and metamorphism. SIMS U-Pb and delta18O depth-profiling and LA-ICPMS REE depth-profiling techniques were...
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| Format: | Others |
| Language: | en |
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University of Ottawa (Canada)
2013
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| Online Access: | http://hdl.handle.net/10393/28734 http://dx.doi.org/10.20381/ruor-12694 |