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Page 1: Geology of the Schist Lake Mandy mines area, · 2014. 6. 12. · L4a H5a L4a M1 H5a B1a H2b I2c H1a H2b H2b V4 V2 L1 L1c L1c H1a M2 M2 M1 H1 H1a H1d H1a H1c M1 H1 H1d H1c H1d L1a

V3

V3

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H1

H1c

H2

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H2b V1a

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H1

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L2a

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V4

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V6

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B1c

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I1a

L3

H1b

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V2a

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I3

H1d

H1d

I1a

H2

H2 H1d

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BIb

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H3a

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I1a

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B1d

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M1

H3a

H3

V5a

L4a

L4a

H1c

H1

H1

V4

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I3

V5a

H2b

I1a

B1d

H2b

L4a

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V5a

L4a

H5a

L4a

M1

H5a

B1a

H2b

I2c

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V4

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L1

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M2

M2

M1

H1

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M1

H1

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H1c

H1d

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H1

H1

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H2b

H3

H2

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SchistMine

MandyMine

77

Lake

Green

PotterBay

CarlisleLake

SCHISTLAKE

SCHISTLAKE

Ross Creek

StittIsland

Lake

Northwest Arm

Burley

C.N.R.

Channing

to Flin Flon

Airfield

C.N.R.

SASK

ATCH

EWAN

MANI

TOBA

SASK

ATCH

EWAN

MANI

TOBA

Green Lake Fault

Burley Lake Fault

East Mandy Road Fault

West Mandy Road FaultRoss Lake Fault

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318 000101°51'0"

101°51'0"

101°50'30"

101°50'30"

101°50'0"

101°50'0"

101°49'30"

54°42

'9"

54°42

'9"

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'39"

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'9"

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'9"

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'9"

54°45

'9"

Preliminary Map PMAP2006-1

NOTE: Darker colours in the legend represent areas of outcrop; lighter colours, areas of overburden.

MISSI GROUP

Pebble to cobble conglomerate, with minor interbedded arkosic sandstone and pebbly arkosic sandstone

Medium to very coarse pebbly arkosic sandstone

M1

M2

+

++

+

Geology of the Schist Lake Mandy mines area, Flin Flon, Manitoba (part of NTS 63K12)

Legend

FLIN FLON ARC ASSEMBLAGE (>1.88 GA ROCKS)Undivided intrusive rocks

c) aphyricb) plagioclase-phyric

Gabbro dikes/intrusionsa) fine to medium grained

a) locally showing screens of the host rock(s)Mafic dike complex

Rhyolite dikes/intrusionsa) quartz-plagioclase-phyric

I1

I2

I3

Undivided volcanic rocks

b) massive flows and mafic sills intercalated with thin intervals of well-bedded mafic tuffa) massive and pillowed flows

a) massive to pillowed plagioclase-phyric flows, locally pyroxene-plagioclase-phyric or aphyric, locally interbedded with well-bedded mafic tuff

a) well-bedded mafic tuffb) plagioclase-crystal-rich tuff

Aphyric to sparsely plagioclase-phyric basaltic flows

Mafic volcaniclastic rocks

Monolithic felsic breccia

Heterolithic breccia composed of mafic and felsic volcanic clasts

Heterolithic mafic breccia

Plagioclase-phyric basaltic flows

V1

V2

V3

V5

V6

V4

INTRUSIVE ROCKS (<1.845 GA)B1

P Phantom Lake intrusionsa) quartz-feldspar porphyry

a) melagabbro, locally with various xenolithsb) hornblende-leucogabbro, pegmatitic in placesc) fine- to medium-grained gabbrod) metapyroxenite

Boundary intrusions

Louis formation

L4

L5

L6

L7

L1

L2

L3

c) mainly pillowed flows

a) massive and pillowed flowsb) massive flows

a) medium- to coarse-grained gabbro, locally plagioclase- and/or pyroxene-phyric

Undivided mafic dikes/intrusions and massive coarse-grained mafic flows

Syn-volcanic mafic dikes/intrusions

Rhyolitea) quartz-plagioclase-phyric

Mafic volcaniclastic rocksa) well-bedded mafic tuffAphyric to sparsely plagioclase-phyric basaltic flows

b) pillowed flowsa) massive and pillowed flowsPlagioclase-phyric basaltic flows

b) massive and pillowed flowsa) thick coarse-grained massive flows with thin pillowed and/or amoeboid breccia topPlagioclase-pyroxene-phyric basaltic flows

Hidden formation

a) quartz-phyricSyn-volcanic felsic dikes/intrusions

Syn-volcanic mafic dikes/intrusionsa) dike swarm with <10% screens of host rock(s)

a) well-bedded mafic tuff, lapilli and brecciaMafic volcaniclastic rocks

b) plagioclase-crystal-rich matrixa) with cored- clastsHeterolithic mafic breccia

e) massive flow showing columnar jointingd) monolithic flow top brecciac) massive and pillowed flows with abundant amoeboid pillow brecciab) massive and pillowed flowsa) mainly pillowed flowsAphyric to sparsely plagioclase-phyric basaltic flowsH1

H2

H5

H4

H3

RoadTrailBridgeRailway

Limit of mappingOutcrop limit

FaultsDefinedApproximateAssumed

Geological contactsDefinedApproximate

AssumedFacies

SymbolsPlanar structure

LineationsFold axis: generation unknownFold axis: generation unknown, symmetricFold axis: generation unknown, S symmetryFold axis: generation unknown, Z symmetryL-fabric: generation unknownSlicken striae

Bedding: tops - unknown, known, overturned

Flow contact: tops - unknown, known, overturnedFoliation: generation - unknown, 1st, 2nd

Fault: sense - unknown, dextral, sinistral

Fold axial plane

Shear zone: sense - unknown, dextral, sinistralShear band: generation unknown, 2nd, sinistral

Pillow: top known

Mafic dikeFelsic dike

Geology by:R.- L. Simard (2006)

Published by:Manitoba Science, Technology, Energy and MinesManitoba Geological Survey, 2006This map is a provisional summary of work carried out during the summer field season and is produced directly from the geologist's manuscript. It is not to be regarded as a final interpretation of the geology of the area.

Cartography by: M.E. McFarlane

SUGGESTED REFERENCE:Simard, R.- L. 2006: Geology of the Schist Lake Mandy mines area, Flin Flon, Manitoba (parts of NTS 63K12); Manitoba Science, Technology, Energy and Mines, Manitoba Geological Survey, Preliminary Map PMAP2006-1, scale 1:5000.

The third (TGI) provides integrated geoscience knowledge pertaining to areas of high base metal potential, with the intent of stimulating private-sector resource exploration. The TGI3 project at Flin Flon is a collaboration of the Geological Survey of Canada, the Manitoba and Saskatchewan geological surveys, Hudson Bay Exploration and Development Company Ltd. and Laurentian University.

Targeted Geoscience Initiative

100 0 100 200 300 400 50050 metres

1:5 000

0 10050 km

62I

63I

62J

62F

64I

52L

52E62H

53J

62P

63J

62K

53F63F

62G

62N

53L

53E

53D63A63C 63B

62O

63H

52M

63P

53K63K

63G

64J

54F64F

53N63N

54L

54A54B54E

54C

53O54D64A64C 64B

63O

54H64H

53M

54G

54K

64P

64K

64G

64N 64O 54M

INDEX MAP

PMAP2006-1

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