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pro vyhledávání: '"T. Ferbey"'
Autor:
A. Plouffe, I. M. Kjarsgaard, T. Ferbey, D.H.C. Wilton, D. C. Petts, J. B. Percival, C. H. Kobylinski, R. McNeil
Publikováno v:
Economic Geology.
At the Gibraltar porphyry Cu-Mo deposit in south-central British Columbia, Canada, geochemical and mineralogical anomalies in till around a cluster of mineral occurrences form amoeboid-shaped dispersal patterns controlled by three phases of ice movem
Akademický článek
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Colour, texture, and chemistry were used to determine the source of tourmaline grains in local surficial (detrital) sediments from two Canadian porphyry systems (Woodjam and Casino). Tourmaline from porphyry bedrock is generally dark brown to black.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7c28fb825b7ccf0382d063b5d8c21a51
https://doi.org/10.4095/327989
https://doi.org/10.4095/327989
Publikováno v:
Economic Geology. 112:919-940
We thank J. Spence for assistance with LA ICPMS analyses. Till collection and sample processing was supported by Natural Resources of Canada Targeted Geoscience Initiative 4 grants to AP and TF. LP was supported by student scholarships from Geoscienc
Autor:
J B Chapman, T Ferbey, MI Leybourne, A M McDonald, A Plouffe, M B McClenaghan, C E Beckett-Brown, M W McCurdy
Tourmaline is considered a potential indicator of porphyry-style mineralization as it is a relatively common accessory mineral and has a broad range of compositions. The aim of this study is to test discrimination criteria for tourmaline in relation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::474cc8c9296c3bdcf3997e9d0596a00f
https://doi.org/10.4095/306427
https://doi.org/10.4095/306427