The hydrothermal and magmatic evolution of the Sturgeon Lake caldera complex is graphically documented by a regional-scale (525 km2) analysis of oxygen...
The Paleoproterozoic Flin Flon mining district is one of the world's most prolific volcanogenic massive sulfide (VMS) camps and includes a single stratigraphic...
A personal computer-based geographic information system (GIS) is used to develop a geographic expert system (GES) for mapping and evaluating volcanogenic...
The massive sulfide deposits of the Kristineberg area, Sweden, occur within a 2- to 3-km-thick succession of felsic volcaniclastic rocks belonging to the...
The Ansil Cu-Zn volcanic-hosted massive sulfide deposit is located approximately 14 km north-northwest of Rouyn-Noranda, Quebec, within the Blake River Group...
Drilling of the active Trans-Atlantic Geotraverse (TAG) deposit during ODP Leg 158 indicated that the size of the mound-stockwork complex is approximately 3.9...
Juvenile 1.89 Ga oceanic arc volcanic rocks of the Flin Flon volcanic belt at Snow Lake are characterized by extensive zones with anomalous 1.82 Ga metamorphic...
Emplacement of the ca. 2735-2720 Ma Sturgeon plutonic suite (SPS) into 2774-2745 Ma oceanic arc crust of the Savant-Sturgeon Lake greenstone belt, western...