Physical Volcanology, Hydrothermal Alteration and Massive ...

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(J)i~"l::.,,",,("'Q""oro Km[TI Late coldero fill 0 ~~~ol;~~~lci~~keScoleaI 7 I" L" Succession [TI ~~~~~~~io~Qkeo Mottobi Succession ~ Precoldero Volcanics[TI Toilings Lake Succession ~ ~~i~:;:eonC:~~lex/D ~ High Level Lake pyroclastic 0 !nt81"J'1:'ediote-mofic~ 5~L..::....Jllow depos;l. ,ntruSlve rocksS 4 4 ....... " O'O' 6 Synvolconic faults --4 Sell late N-S faults -----( ~ ~ 3 • 5 b 5 ~~ Uoss;"e sulph;de depos;(s_1-----4 U ~, 0 ~ ~- 0°00000- UO? -'" .....o Ou O 0 0 0 0'0°6OOOOOOOOOOOOOUOOOO C ·00000 °8eldlem~n Bay
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Page 6 and 7: 95°HudsonBaySioux~LOOkoutSturgeonL
Page 8 and 9: ounded to the north by the English
Page 12 and 13: mosaics. The ash-size matrix is com
Page 14 and 15: eruptive cycle and are overlain by
Page 16 and 17: are found throughout the lateral an
Page 18 and 19: gradual change from rhyolitic quart
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Page 22 and 23: 55%) in 1-5 mm wide grey-green vein
Page 24 and 25: !Sturgeon LakeSCALE500....TLEGEND O
Page 26 and 27: FIELD TRIP STOP DESCRIPTIONSF-Group
Page 28 and 29: Stop F-1: High Level Lake Ash Flow
Page 30 and 31: Stop F-3: Mesobreccia- High Level L
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Page 34 and 35: massive chloritic veining up to 50
Page 36 and 37: generally aligned in the strike dir
Page 38 and 39: This spectacular volcanic breccia i
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Page 43: WINNIPEG'96 GUIDEBOOK ORDER FORMA1.

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