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Tungsten Mineralization Processes at the Sisson Brook W‐Mo‐Cu deposit, Central New Brunswick: the Role of Formation of Titaniferous Phases at Reaction Fronts

Tungsten Mineralization Processes at the Sisson Brook W‐Mo‐Cu deposit, Central New Brunswick: the... June 2013 BUSTARD Aaron, ZHANG Wei, MCFARLANE Christopher R.M and LENTZ David 2013. Tungsten Mineralization Processes at the Sisson Brook W-Mo-Cu deposit, Central New Brunswick: the Role of Formation of Titaniferous Phases at Reaction Fronts Acta Geologica Sinica (English Edition), 87(supp.): 672-675. Tungsten Mineralization Processes at the Sisson Brook W-Mo-Cu deposit, Central New Brunswick: the Role of Formation of Titaniferous Phases at Reaction Fronts BUSTARD Aaron*1, ZHANG Wei1, MCFARLANE Christopher R.M.1 and LENTZ David1 University of New Brunswick, Fredericton, N.B., Canada, E3B 5A3 Sisson Brook is a large tonnage, low grade W-Mo-Cu deposit located in west-central New Brunswick, Canada (see Zhang et al., this volume). The deposit is one of several in New Brunswick associated with the intrusion of granitic plutons related to the Devonian Acadian orogeny. These deposits include Mount Pleasant (W-Mo), Lake George (Sb& W-Mo-Au), and Burnthill (W) (Ruitenberg and Fyffe, 1991). This integrated petrologic study included analysis by optical microscopy, scanning electron microscopy-backscattered electron imaging (SEM-BSE), and in-situ laser ablation inductively coupled plasma-mass spectrometry (LA ICP-MS) with the goal of determining the influences of titaniferous phases on the distribution of W mineralization. LA ICP-MS was also used to date the weakly foliated Howard Peak metadiorite http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Geologica Sinica (English Edition) Wiley

Tungsten Mineralization Processes at the Sisson Brook W‐Mo‐Cu deposit, Central New Brunswick: the Role of Formation of Titaniferous Phases at Reaction Fronts

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Publisher
Wiley
Copyright
© 2013 Geological Society of China
ISSN
1000-9515
eISSN
1755-6724
DOI
10.1111/1755-6724.12149_5
Publisher site
See Article on Publisher Site

Abstract

June 2013 BUSTARD Aaron, ZHANG Wei, MCFARLANE Christopher R.M and LENTZ David 2013. Tungsten Mineralization Processes at the Sisson Brook W-Mo-Cu deposit, Central New Brunswick: the Role of Formation of Titaniferous Phases at Reaction Fronts Acta Geologica Sinica (English Edition), 87(supp.): 672-675. Tungsten Mineralization Processes at the Sisson Brook W-Mo-Cu deposit, Central New Brunswick: the Role of Formation of Titaniferous Phases at Reaction Fronts BUSTARD Aaron*1, ZHANG Wei1, MCFARLANE Christopher R.M.1 and LENTZ David1 University of New Brunswick, Fredericton, N.B., Canada, E3B 5A3 Sisson Brook is a large tonnage, low grade W-Mo-Cu deposit located in west-central New Brunswick, Canada (see Zhang et al., this volume). The deposit is one of several in New Brunswick associated with the intrusion of granitic plutons related to the Devonian Acadian orogeny. These deposits include Mount Pleasant (W-Mo), Lake George (Sb& W-Mo-Au), and Burnthill (W) (Ruitenberg and Fyffe, 1991). This integrated petrologic study included analysis by optical microscopy, scanning electron microscopy-backscattered electron imaging (SEM-BSE), and in-situ laser ablation inductively coupled plasma-mass spectrometry (LA ICP-MS) with the goal of determining the influences of titaniferous phases on the distribution of W mineralization. LA ICP-MS was also used to date the weakly foliated Howard Peak metadiorite

Journal

Acta Geologica Sinica (English Edition) – Wiley

Published: Jun 1, 2013

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