The 370 Ma peraluminous South Mountain Batholith (SMB) intrudes Meguma Supergroup
metasedimentary rocks in Nova Scotia. The New Ross area of the SMB contains …

The most evolved rocks of the South Mountain Batholith host polymetallic (Sn-WU-Mo-Cu-
Mn) mineral deposits in the New Ross area (NRA). This project presents new data (fluid …

Abstract The West Gore Sb-Au deposit is anomalous in the Megurea terrane of Nova Scotia
because of its enrichment in Sb, a metal that is essentially absent from other Megurea gold …

Mineral exploration in areas of little bedrock exposure must increasingly rely on the
predictive quality of geological, geochemical and geophysical data. In this contribution …

Mineral thermometry and fluid inclusion studies were conducted on variably altered and
mineralized samples from the Mesoproterozoic Pea Ridge iron oxide-apatite (IOA)-rare …

Thermometric and salinity data are presented for fluid inclusion populations in samples of
hydrothermal vein material (quartz intergrown with wolframite, cassiterite, stannite …

The 404Ma Rosses Granite Complex is a member of the late-Caledonian Donegal Granites
of NW Ireland. The Rosses Complex comprises an annular assemblage of four nested …

The bulk composition of fluid inclusions is generally determined by using the temperature of
ice melting (ie, freezing-point depression of H2O–NaCl) and relating this to the ice-melting …

Three distinct types of fluid inclusions (ie, liquid+ vapor (LV), liquid+ vapor+ solid (LVS), and
V-only) co-exist within a single, primary fluid inclusion assemblage in fluorite crystals that …

Granitic rocks in the New Ross area, Nova Scotia, host polymetallic (Cu, Mo, Mn, Sn, U, W),
aplite–pegmatite, greisen, and vein-type mineral deposits. The host granitic rocks belong to …