Geochemical characteristics of biotite from felsic intrusive rocks around the Sisson Brook W–Mo–Cu deposit, west-central New Brunswick: An indicator of halogen and …

W Zhang, DR Lentz, KG Thorne, C McFarlane - Ore Geology Reviews, 2016 - Elsevier
Abstract The Sisson Brook W–Mo–Cu deposit was formed by hydrothermal fluids likely
related to the Nashwaak Granites (muscovite–biotite granite, Group I; and biotite granite …

Chemical composition of biotite from the Casino porphyry Cu–Au–Mo mineralization, Yukon, Canada: evaluation of magmatic and hydrothermal fluid chemistry

D Selby, BE Nesbitt - Chemical Geology, 2000 - Elsevier
The chemical composition of biotite has been determined for the Dawson Range batholith
and the Casino, porphyry-style Cu–Au–Mo occurrence, Yukon Territory, Canada. Biotite …

Using magmatic biotite chemistry to differentiate barren and mineralized Silurian–Devonian granitoids of New Brunswick, Canada

Z Azadbakht, DR Lentz, CRM McFarlane… - … to Mineralogy and …, 2020 - Springer
The geochemistry of biotite crystals from thirty fertile and barren Silurian–Devonian
granitoids of New Brunswick, Canada, was studied in situ using electron microprobe and …

Geochronology and geochemistry of the MAX porphyry Mo deposit and its relationship to Pb-Zn-Ag mineralization, Kootenay arc, southeastern British Columbia …

CJM Lawley, JP Richards, RG Anderson… - Economic …, 2010 - pubs.geoscienceworld.org
The MAX porphyry Mo deposit is located at the northern end of the Kootenay arc in
southeastern British Columbia, Canada. Molybdenum mineralization is genetically related to …

Volcanic-hosted rare-metals deposit at Brockman, Western Australia: mineralogy and geochemistry of the Niobium Tuff

AR Ramsden, DH French, DI Chalmers - Mineralium Deposita, 1993 - Springer
Rare-metals mineralization at Brockman, Western Australia, is the product of early
pyroclastic eruption of trachytic magma enriched in volatiles and incompatible elements …

Petrography and mineral chemistry of the composite Deboullie pluton, northern Maine, USA: Implications for the genesis of Cu Mo mineralization

PJ Loferski, RA Ayuso - Chemical Geology, 1995 - Elsevier
Biotite and apatite mineral chemistry, particularly halogen abundances and ratios, are used
to investigate the relation of the two contrasting parts of the Deboullie composite pluton …

Petrology and Li-Be-B geochemistry of muscovite-biotite granite and associated pegmatite near Yellowknife, Canada

R Kretz, J Loop, R Hartree - Contributions to Mineralogy and Petrology, 1989 - Springer
Abstract Prosperous granite (Rb-Sr 2520±25 Ma) occurs as several plutons (1–380 km 2
outcrop area) in a thick succession of metamorphosed greywacke-mudstone of the …

Mica chemistry as an indicator of oxygen and halogen fugacities in the CanTung and other W-related granitoids in the North American Cordillera

WT Van Middelaar, JD Keith - 1990 - pubs.geoscienceworld.org
In this chapter we report on the use and limitations of oxygen and halogen fugacities to
characterize granitoids associated with tungsten deposits. Tungsten-related granitoids …

Protracted magmatism and mineralized hydrothermal activity at the Gibraltar porphyry copper-molybdenum deposit, British Columbia

C Kobylinski, K Hattori, S Smith… - Economic …, 2020 - pubs.geoscienceworld.org
Abstract The Gibraltar Cu-Mo deposit, with a total tonnage of 3.2 million tons (Mt) Cu, is
located in the Canadian Cordillera and hosted by the Late Triassic Granite Mountain …

Magmatic–hydrothermal fluids and volatile metals in the Spirit Lake pluton and Margaret Cu–Mo porphyry system, SW Washington, USA

AA Iveson, JD Webster, MC Rowe, OK Neill - Contributions to Mineralogy …, 2016 - Springer
The halogen-bearing minerals tourmaline, amphibole, and biotite formed during magmatic–
hydrothermal processes associated with the late-stage cooling of the Spirit Lake granitoid …