Interaction of magmatic fluids and silicate melt residues with saline groundwater in the footwall of the Sudbury Igneous Complex, Ontario, Canada: New evidence from bulk rock geochemistry, fluid inclusions and stable isotopes

Author:

Hanley Jacob,Ames Doreen,Barnes Jaime,Sharp Zachary,Guillong Marcel

Funder

Swiss Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference135 articles.

1. The supergiant Ni–Cu–PGE Sudbury district, Ontario, Canada;Ames,2007

2. Sudbury Targeted Geoscience Initiative (TGI): role of volatiles, structure and host rocks in the evolution of Sudbury ores;Ames,2001

3. Behaviour of trace elements during magmatic processes: a summary of the theoretical models and their applications;Arth;US Geol. Surv. J. Res.,1976

4. The magmatic-hydrothermal evolution of two barren granites: a melt and fluid inclusion study of the Rito del Medio and Cañada Pinabete plutons in northern New Mexico (USA);Audétat;Geochim. Cosmochim. Acta,2003

5. The composition of magmatic-hydrothermal fluids in barren and mineralized intrusions;Audétat;Econ. Geol.,2008

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