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 …

Abstract The 391.2±3.2 Ma (U-Pb on zircon) Evandale Granodiorite of southwestern New
Brunswick is quite a unique intrusive rock in the southern part of the northeastern …

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 …

A numerical method is presented to estimate the crystallization pressure of granite intrusions
based on two polynomial equations obtained by an analysis of the existing haplogranite …

We have compiled whole-rock analyses in mantle rocks to investigate the abundance of
gold in the lithospheric mantle, and how this distribution can be modified. We show that …

Increasing the prediction rate in the identification of mineralization zones using the stream
sediment geochemical data is an essential issue in the regional exploration stage. The …

A-and I-type magmas are commonly associated with rare earth element (REE) and gold (Au)
mineralization. However, the behavior and solubility of the REEs and gold within the A-and I …

The geochemistry of apatite crystals from fifteen fertile and infertile Acadian-related
granitoids of New Brunswick (Canada) was studied in situ, using electron microprobe and …

This study uses selected granite samples to evaluate the effect of redox conditions
expressed as molar ferric-ferrous iron oxide ratio, Fe 3+#[= Fe 2 O 3/(FeO+ Fe 2 O 3)], on …

Cenozoic magmatism in Iran is associated with many epithermal-porphyry Cu-Au ore
systems, which mainly occur within the Alborz Magmatic Arc and Urumieh-Dokhtar …