Physical Volcanology, Hydrothermal Alteration and Massive ...
Physical Volcanology, Hydrothermal Alteration and Massive ...
Physical Volcanology, Hydrothermal Alteration and Massive ...
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STURGEON LAKEN/o POST -CALDERA VOLCANICS00 MASSIVE SULPHIDE DEPOSITS~ CALDERA RElA1ED VOLCANICS~ PRECALDERA VOLCANICSo lRONDHJEMITIC IN1RUSIVES1Zl FAULTSB CON1ACTSFigure 2. Generalized geological map illustrating the regionalextent of the sturgeon Lake Caldera Complex.The combination of well preserved volcanic textures, a variable 55 0 to 90 0 dip ofa north-facing, essentially homoclinal volcanic sequence <strong>and</strong> more than 600,000 m ofdiamond drilling over an apparent 4,500 m stratigraphic interval presents the opportunityto examine successive stages of caldera evolution. This includes initial subaerial-shallowsubaqueous collapse, subaqueous silicic explosive volcanism <strong>and</strong> ore formation, <strong>and</strong>terminal dome building with sedimentary <strong>and</strong> lava flow fill <strong>and</strong> burial.The main purpose of this field trip is to illustrate the physical volcanology of anancient, ore-hosting caldera <strong>and</strong> to stress the importance of volcanism <strong>and</strong> synvolcanicstructures in controlling the occurrence <strong>and</strong> location of hydrothermal alterationassemblages <strong>and</strong> volcanogenic massive sulphide deposits.REGIONAL GEOLOGYThe south Sturgeon Lake area is located within the Archean Wabigoon volcanosedimentarygreenstone belt within the Superior Province. The Wabigoon subprovince is3