Several pyritic massive sulfide deposits have been recognized in an Ordovician-Silurian volcano-plutonic complex in the southern Prince of Wales Island region (Fig. 1). These deposits have been studied as part of a U.S. Geological Survey-California Institute of Technology investigation into the geologic and mineralization history of southern Prince of Wales Island (south of 55° North Latitude; Fig. 1). This report describes the geologic setting of the deposits and presents preliminary chemical analyses of the mineralization
The Greens Creek Zn-Pb-Ag-Au volcanogenic massive sulfide (VMS) deposit is located on Admiralty Isla...
The Waterloo massive sulfide deposit occurs in the Cambro-Ordovician Seventy Mile Range Group in the...
The Waterloo massive sulfide deposit occurs in the Cambro-Ordovician Seventy Mile Range Group in the...
Several pyritic massive sulfide deposits have been recognized in an Ordovician-Silurian volcano-plu...
Geologic mapping on southern Prince of Wales Island combined with U-Pb (zircon) geochronologic, geoc...
Geologic mapping on southern Prince of Wales Island combined with U-Pb (zircon) geochronologic, geoc...
The Klakas orogeny is a Late Silurian-Early Devonian deformational, metamorphic, and mountain-buildi...
The Prince William Sound region is located approximately 100 km east-southeast ofAn-chorage, Alaska,...
Pilley's Island in the Central Mobile Belt, Newfoundland, Canada, is host to a cluster of bimodal fe...
Geologic mapping, U–Pb (zircon) geochronometry, and conodont studies indicate that the major pre-Jur...
The Neoproterozoic Alexander terrane Niblack Cu-Au-Zn-Ag volcanic-hosted massive sulfide camp is on ...
The focus of this study is the Betts Cove massive sulphide deposit which is located within the Betts...
The Snowdon caldera of North Wales is host to base metal sulfide-bearing veins and stockworks, miner...
The Neoproterozoic Alexander terrane Niblack Cu-Au-Zn-Ag volcanic-hosted massive sulfide camp is on ...
The Greens Creek Zn-Pb-Ag-Au volcanogenic massive sulfide (VMS) deposit is located on Admiralty Isla...
The Greens Creek Zn-Pb-Ag-Au volcanogenic massive sulfide (VMS) deposit is located on Admiralty Isla...
The Waterloo massive sulfide deposit occurs in the Cambro-Ordovician Seventy Mile Range Group in the...
The Waterloo massive sulfide deposit occurs in the Cambro-Ordovician Seventy Mile Range Group in the...
Several pyritic massive sulfide deposits have been recognized in an Ordovician-Silurian volcano-plu...
Geologic mapping on southern Prince of Wales Island combined with U-Pb (zircon) geochronologic, geoc...
Geologic mapping on southern Prince of Wales Island combined with U-Pb (zircon) geochronologic, geoc...
The Klakas orogeny is a Late Silurian-Early Devonian deformational, metamorphic, and mountain-buildi...
The Prince William Sound region is located approximately 100 km east-southeast ofAn-chorage, Alaska,...
Pilley's Island in the Central Mobile Belt, Newfoundland, Canada, is host to a cluster of bimodal fe...
Geologic mapping, U–Pb (zircon) geochronometry, and conodont studies indicate that the major pre-Jur...
The Neoproterozoic Alexander terrane Niblack Cu-Au-Zn-Ag volcanic-hosted massive sulfide camp is on ...
The focus of this study is the Betts Cove massive sulphide deposit which is located within the Betts...
The Snowdon caldera of North Wales is host to base metal sulfide-bearing veins and stockworks, miner...
The Neoproterozoic Alexander terrane Niblack Cu-Au-Zn-Ag volcanic-hosted massive sulfide camp is on ...
The Greens Creek Zn-Pb-Ag-Au volcanogenic massive sulfide (VMS) deposit is located on Admiralty Isla...
The Greens Creek Zn-Pb-Ag-Au volcanogenic massive sulfide (VMS) deposit is located on Admiralty Isla...
The Waterloo massive sulfide deposit occurs in the Cambro-Ordovician Seventy Mile Range Group in the...
The Waterloo massive sulfide deposit occurs in the Cambro-Ordovician Seventy Mile Range Group in the...