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1:50 000 DEASE LAKE - LITTLE TUYA RIVER GEOLOGY QUEST-NORTHWEST PROJECT NTS SHEETS 104J/08, 07E Location Map
400000 130°40'W 130°35'W 410000 30' 130°25'W 420000 130°20'W 15' 430000 130°10'W 130°5'W 440000 A YUKO
) ) N TERRITORY
( ) ) 0 1 ) 0 Ï ) 3 ( ) ) ) 3 ! 44 0 ) ) 57 ( ) ) ) 1 55 ! 0 ) JIs ( ) ) ) ) Ï U K i n g ) 28 .
) 65 ) 46 D e a s e 65 S ) ( ! .
) ! ( 40 L a k e A
) ) ) ( F 54 . Dease Lake ) ) % ! ) ) ) Ï ( ( Ï ) ) 70 51
) ) ! 50 ( T Ï ) ) ( a ) 35 fp 34 t ) ) LJqfp ( q ! s ) ) ) ) ! ( J h ( L 9 o 0 A 0
63 0 L ! BRITISH COLUMBIA 0 C
4 ! 75 ( ( r B
1 67 e
A e
k E
60 p 80 ( Ï 1 JIs
f ! 0
R ! 75 ! q ( 56 0 ! J 0 Map Area
L ( ! Qal T A
60 60 Ï 44 !
! ( (
0 18
0 ø A Ï 4 ! ( JIs 44 38 22 66 eJTcs 1 55 70 ( Ï ! 70 ( 68 65 70
1 40 68
0 7 ( Ï 0 ( 24 Ï ! Ï
0 104J 064 ( PzTrCClw
63 q ! 50 ! Ï 42 Qal ! ( 30
7 P(zTrCC(lw 66 ! 60 Ï ! Prince ( ( Ï 20 Ï 60 !
( 46 George k Ï
73 Ï Ö 88
e 104K 154 eJTcs ( PzTrCCum Ï Ï
k ( !
e e Ï E ( Ï
0 74
r e Ï 15 0 ( ø r 44 7 43 !
1 l 20 ) C Ï 15 55 C ! C ) 17 ( C ) r 83 k 52 zT l 85 ) 30 s P C
c 85 40 ) Ï
s ( rC S Ï
Ï a ! P
o o Ï Ï T l ) 37 z m MPlTv 1 (! 1 PaSPgd ) Ï a s P 65 o R ( n 0 c ) 0 s ) 8 i 1 ( Ï PzTrCCv Qal 0 f e 8 i
) 0
0 81 c k ( 0 0 70 ! 64.5±0.3 Ma ) 104J 014 Ð 0 O c ( 80
47 8
1200 ) Ï 57 c
"S ( ) 4
M ½ e
½ Re H 6
½ ( )
½ PzTrCCl 40 a ½ (
½ *, 1
½ ( ! 46
½ 60 n
5 ( o
½ p ( ! Ï ½ Ï
½ ( 66
f 63.5±0.4 Ma 0 (
½ ( ½ 0 t
½ q Z Ï ½ (
½ (
J *, ( ( ( 1(52.0±1(.1 Ma ( 1 Ò lTrSc e !
17 ( 0 Vancouver ½
½ ( ( ( Z 62 ( A. L 0 . S. ! 0 ( U ! ( ( ( *, ( C 41 ( ( ( ( A ( 0 0 eJTcs
(( ( 45 r e
0 lTrS? 58 ( e
0 PzTrCClw k B ( ( VICTORIA
8 lTrSc
Ï ( ( ( ( Ï \
Ï ( ( Ï 28
4 lTrSpp (33 (40 ( ( ( Ö ( ( Ï
S Ï
6 PzTrCClw 3 ( ( ( ( ( lTrSc
3
½ i
½ ( (
½ F (
46 ½ x a 40 ½
45 u !
½ l
89 ½ PzTrCClw t 54
½ JIs
½ 73 t 84 65 ½ )
3 )
½ Ï ) ) !
½ e
Ï
½ !
½ ) )
½ 60 e
½ 0
) )
0 7 25
½
½ n
)
6 ) )
40 )
1 7 ! M 0
) 56 110 ) 7 ) i l p ! ) e f 35
eJTl !
q Dease )
C Ï )
r e J
1 e )
k Ï L ) Lake
5 Ï 66 !P
0 lTrSc
)
eJTcg lTrSc )
0 ) Previous Mapping in the Region
½ !P
½ )
½
½ 25
½
½
½
!
½ 37
½ )
A ) JIs
½ 40 Ï 48 )
½ Ï
½ ) ) ½ ½ A Ï ½ ½ lTrSc 132°W 130°W 128°W Ð
½ !
½ )
lTrSpp 55 ! ! 52 61 ! 60 65 85 )JIs
25 35
24 ! ! 50
lTrSpp Ï ! 56
! B 0
0
0
65 1 ½
½
½
½
½
½
½ 30 74 ½
½ ½
!
½ 0
½ ½
½ Ï 0 ½ ½ 8 ½
½ Ï 55 ! lTrScg
rt 3 27 po 16 25 eJTcs ir 45 A
48 1
Ï 90 A 1
6 eJTcg 3 eJTcg 2
0
0
0 75
½ 0
Ï ½
½ 63
½ F Dease
E E E ½ E E E E E 58°25'N
58°25'N ½
½ !P
½ *,
½
½ F 3
½ Lake ½
½
 3 40 *, ½
½
½ ½ ½ ½ ½ ½ ½ 3 3 Ï
! Golden
34 #* #* Major mineral deposits
40 Bear Gnat 34 Ð #*
50 6 lTrScg
Ï Pass 0 ! r Kutcho
0 Parks
0
0 #*
54 8 e
26 Ö
5 Ï 60 75 70 Creek
1 0 v
½ 58°N
½ 0
½ 3 i
8 ½ 1
½ 1
0 ½ This study ½
½
0 ½
½ R
!
½
½
48 ½
½
½ 25
½ 46 ½ ½
½ ½ Ï Telegraph ½ ½ !
! a !P 58°N 19 60 q l Previous Mapping
! Ö l Creek
23 lTrScg i
Ï 20 z !P Iskut Moynihan and Logan, 2012
lTrS ! n
! 21 a
35 ! 53 20 ! T
½ 67 Red
½ !
½ van Straaten et al., 2012
½
½ #*
½ Ma ½ 80 179.5±1.8
½
½ Ar #* GJ Chris ½
½
½
½ lTrSpx *, 0
½
½ 0 ½ 2
½ ½ 1 Anderson, 1983 ½ ½ ½ ½ 35 22 ! !
32 40 Ash et al., 1997 ! 45
20 ! ! ! #* Schaft
lTrSpx Ï
eJTcg ! Creek Brown et al., 1996
½ 37
lTrS ½ ½
½
Ð
½
½ B ½
½
½
½ 30
½ 40
½ d l e ! Ï Evenchick and Thorkelson, 2005
½ i
½ h C ½ c r e
½ g u s e k 75 87 86 Galore
u 17 ! #* A ! ! Creek ! Gabrielse, 1998 30 Read, 1983, 1984
8 37 0
0 65
½
½
½
½
½
½
½
½ 0 Qal Read and Psutka, 1990
½ 72 Ï 0 ½ 8
½ 132°W 130°W 128°W ½ ½ ½ Ï
MPlTv ½ ½ !P
#* #*
½ Qal Note: Outcrops are shown with a darker shade
½ 0
13 ½ 0 ½
0 ½
½ 0
½
½
½ 38 0
½ 7 MPlTv ½ #*
½ 0 ½ PLEISTOCENE AND RECENT ! 0 0 ½ ½ ½ 7
35 4 ! Unconsolidated glacial, lacustrian, alluvial and colluvial material. 6 Qal 65 lTrSpp Ï
Ò 20 MIOCENE TO PLEISTOCENE
!
0 Ï 30
0
½ Tuya Formation
½
0 ½
½
½
0 ½
½ Ï
½
½ Alkali olivine basalt; grey to brown coloured, columnar-jointed. Yellowish green, mm-size phenocrysts of olivine and vitreous plagioclase ! 7 ½
½ ½
4 ½ ½ MPlTv ½ 75 ½ in a fine grained groundmass.
6
Û 30
47 42 ! ! 7Ï 8 !
66 38
Ï ! F EOCENE
Qal 65 44 75 !
*, 30 1 Tanzilla Canyon Formation 3 35 ! lTrSvs !
45 55 ! 0
62 ! 0
! 40 Poorly consolidated conglomerate, sandstone and mudstone; marl and lenses of high-volatile B bituminous coal.
½
½ ETCcg
T ½ 36 ½
½ q
½
!
½ !
½ ! 27 lTrScg ½
u ½
½ 10 MJHgd 40 ½ #
½ ½ ½ 34
y ½ ! PALEOCENE MPlTv a ! !
lTrSpp I 1200 20 Snow Peak pluton
R t s q ! 104J 013 65 30 ! i 70 ! i l "S Biotite-K-feldspar plagioclase monzonite to syenite; pink weathering, equigranular to porphyritic Laser ablation U-Pb zircon l i lTrScg q lTrSvs 35 PaSPgd
v t u 60 70 Ï 46 crystallization age of 63.5±0.4 Ma; Re-Os molybdenite age for mineralization of 64.5±0.3 Ma.
A lTrSvs
!
e
C ½
½ 900
½
½
r ½
½
½ ½
½ ½ ½ ½ LATE JURASSIC
r 166.5±0.7 Ma ½ ½ ½
½ ½
½ ½
½
½ e ½ ½ ½ MJHsy 75 ½ ½ e Dikes and sills of quartz-hornblende-plagioclase porphyry (QFP); cross cut folded and foliated sedimentary rocks of the Takwahoni 70 *,Z Ï lTrScg LJqfp k q Formation, the King Salmon Fault and mafic volcanic rocks of Cache Creek Terrane. Laser ablation U-Pb zircon crystallization age of 212.2±1.8 Ma TrJgb *,Ar 152.0±1.1 Ma.
58°20'N E E E E lTrScg E lTrSpp E E E 58°20'N
½ lTrSmv
½
½ STIKINE TERRANE
½
½
½ 1
½ ½ ½
½ 1
½ ½ ½
½ ½ 0 ½
½ 0 ½ ½ ½ ½ MIDDLE JURASSIC
½
½ 3 ½ 60 Hluey Lake pluton 1 C 10 y r 0 e e e Biotite-K-feldspar-plagioclase monzonite to syenite; pink weathering, equigranular to porphyritic. Laser ablation U-Pb zircon u k MJHsy l crystallization age of 166.5±0.7 Ma and an incongruous older Ar-Ar biotite cooling age of 212.2±1.8 Ma. H 78
1
½ 2 Biotite-hornblende granodiorite; medium grained, equigranular to weakly foliated at eastern margin.
½ Ï ½
½ 0 lTrSpp
½ MJHgd
½ lTrSpp lTrSpp
0 ½
½ ½
½ ½
½ ½
½ ½
½ ½ ½ ½ ½ ½ ½ 54 ! Pallen Creek pluton 1 Ð 0 F lTrSvs 80 0 Biotite-hornblende quartz monzonite to monzodiorite; equigranular to locally K-feldspar megacrystic. Laser ablation U-Pb zircon
*, 0 MJPm
40 H l u e y L a k e s crystallization age of 172.2±1.0 Ma. ! ! lTrSvs
32 34
!
q 63
! 30 EARLY JURASSIC
60 ½
½ A 30
½ ! f
½ 75
½ 39
f
½ q lTrSvs 32
½ !
!
½
½ Takwahoni Formation
½
½ Ð
½ ½ 9 ½
½ 00 r 45
½ ½ ½ ½ ½ ½ e ½ ½ lTrSw ½
½ ! Undivided sandstone, siltstone, mudstone, greywacke and conglomerate; dark grey to orange weathering, calcareous matrix.
v 1300 80 eJTcs
i 70 q 40 15 55 48 Ï ! 88 ! R TrJgd eJTl Limestone, sandy limestone. The mapped occurrence of this unit is too small to be visible at this scale. The occurrence is denoted by lTrS a F lTrSw outcrop location (x). l TrJgb *,
i l 00
n z lTrSw 12 80 Basal unit of coarse polylithic conglomerate, coarse sandstone and lesser siltstone.
! eJTcg
!
½ a 85 Ï
½ 104J 036 ½
½ ½ ½ ½ ½ T !
½ 80 TRIASSIC TO JURASSIC lTrSw lTrSw lTrSw White weathering, equigranular to porphyritic hornblende-plagioclase monzodiorite to granodiorite; acicular 1-8 mm hornblende Ï 0 TrJgd 0 1 TrJgd crystals±biotite in a fine grained feldspar matrix. 75 1 v T r Pyroxenite, hornblende gabbro, diorite and monzodiorite intrusive complex; high magnetite content of intrusions is reflected by high
T TrJgb
m 32 ! ½ magnetic susceptibility and corresponding high aeromagnetic signature. ½ ½ 0 45 0 ! 0 0 2 Ï 0 1
1 70 LATE TRIASSIC 3 60
70 0 lTrSvs
0
Ï B Ï Stuhini Group
4
1 ½ ½ ½ ½ 35 ½ Undivided coherent volcanic flows, clastic and sedimentary rocks. mTrTv S i t s a lTrS
0 0 L a k e 6 ! Mafic volcanic-dominated polylithic conglomerate, sandstone and greywacke; massive, rarely bedded, weathers orange and includes ! mTrTv lTrScg 172.2±1.0 Ma 1 lTrSpp 3 ! rare augite phyric basalt flows. ! 0 0 0
0 Z 0 0 ! Ï
3 *, 0 Augite±plagioclase phyric basalt; primarily thick monomict breccias, massive coherent flows and rare pillowed forms, 4-10 mm euhedral
1 ( 67 ! lTrSpx
Qal 0 6 black augite phenocysts in a pale green finer grained groundmass. ½ ½ ½ ½ ! ! (
MPlTv 4 TrJgb !
6 Latite, K-feldspar phyric trachyte, vesicular pyroxene basalt and minor volcanic sandstone; maroon to purple, friable.
ePSl 40 ( 48
Ï lTrSw lTrSmv ePSv % 40 Ï ! ! ( 15 1 0 6 Plagioclase±augite phyric basalt flows; green, grey and massive, 2-8 mm white plagioclase phenocrysts, often glomeroporphyritic in a 0 Qal T h i r t y M i l e 0 ! 0 30 0 lTrSpp ( 0 L a k e fine grained green groundmass. ! MPlTv lTrSw 6
4 ( ! 0
6 ! 15 0 Well-bedded, volcanic sandstone, siliceous siltstone and subordinate conglomerate; pale green, grey and orange, contains Upper 3
! ! lTrSvs ! 1
700 ( 12 ! Triassic bivalves and conodonts (M. Orchard pers comm., 2012).
60 14 MPlTv Ï
! ePSs !
( ! ! Z
0 Z ! 74 ! MJPm Volcanic clast-dominated conglomerate; contains horizons with limestone, chert and siltstone clasts, chaotic, massive to weakly bedded
0 60 ! lTrSw
( 4 40 Ï 1 TrJgd and internally graded.
I 3 F ! 30
48 *, MPlTv
67 ! ePSs ePSl EARLY-MIDDLE TRIASSIC !
! 3! 5
68 50 Î B Ï TrJgd Tsaybahe 'group' Ï 65 !
I ! B
! Coarse augite±plagioclase phyric basalt breccias and flows; orange to grey-green weathering.
28 TrJgd mTrTv !
F A
6 !
*, 34 85
ETCcg ! ! !
e! mTrTa A ! 16 0 Well-bedded, siliceous siltstone, argillite and limestone. Correlative rocks south of map area contain Middle and Early Triassic 104J 044 54 % 73 0 emTrTa 7
1 conodonts (Read, 1984). 28 50 9 64 ! "S E E 15' 400000 130°40'W 130°35'W 410000 30' 130°25'W 420000 130°20'W 15' 430000 130°10'W 130°5'W 440000 PERMIAN Stikine Assemblage Limestone; cream to grey coloured, well-bedded and interlayered with irregular black and grey chert nodules and layers. ePSl
Siliceous siltstone; green and buff coloured, interlayered and gradational into grey and maroon chert. ePSs
Plagioclase phyric lapilli tuff and breccia; penetratively foliated, maroon and green, carbonate altered. ePSv
Station Distribution with Geological Line Features QUEST-Northwest Total Field Magnetics (Aeroquest Airborne, 2012) with Geological Line Features and Altered/Mineralized Rock Sample Locations CACHE CREEK TERRANE EARLY JURASSIC 400000 410000 420000 430000 440000 400000 410000 420000 430000 440000 Inklin Formation ( ) ) ) ( ) ) ) ) ) ) ) ) ( ) ) ) ) ) Phyllite, phyllitic greywacke, siltstone with minor limestone and conglomerate; grey-green and calcareous. Possibly lateral fine grained ) ( ) ) ) ) ) ) ) JIs ) ) ) (( ) ) ) (( equivalent to coarser Takwahoni Formation overlying Stikine Terrane. ) ) ) ) ( ) ) ) ) ( ! ) ) ) ) ) ) ) ( ( ) ) ) ( ( LATE TRIASSIC Sinwa Formation ( ( ( ( ! Marble; grey, white and massive, forms structureless isolated exposures, locally foliated and rarely fossiliferous. Typically a light brown lTrSc amorphous rock cut by a dense stockwork of white calcite veins. ( ( ( ( ( (
7 7 MISSISSIPPIAN TO TRIASSIC ( ( ( ( JLO-12-105 ( ( ( ( Cache Creek Complex ( ( ( ( PzTrCCl Marble; white, grey and black, medium bedded; thinly foliated, locally interlayered with yellowish chert and tuffaceous beds. ) ) ) ) ( ) ( ) ) Meta-basalt; dark green, aphyric to fine pyroxene porphyry, pervasively fractured and penetratively foliated; metamorphic assemblage ) 0 ( 0 ( 0 ( ) 0 ( ) PzTrCCv 0 0 includes epidote, chlorite, calcite and pyrite. 0 ( ) 0 ( ) 8 ) 8 )
( 4 ( ( 4 ( ( Peridotite; dun-weathering, variably serpentinized chrome spinel-bearing; a probable serpentinized dunite(?) at the southern margin is ( 6 ( ( 6 ( ( 0 0 ( ( ( ( ( ( ( ( ( ( PzTrCCum 0 0 ( ( ( ( ( ( ( ( ( ( JL(O-2(9-296-3 thoroughly serpentinized and highly magnetic. 0 0 ( ( ( ( 0 0 ( ( ( (
8 ( 8 ( ( ( ( ( ( ( ( ( ( ( (
( 4 4 ( ( Listwanite altered ultramafic rocks comprised of quartz-talc-carbonate-chrome mica and locally pyrite. The unit crops out along trace of
6 (
6 ( ) ) JLO-8-65 ) )
) ) ) ) King Salmon Fault. For those mapped occurrences of this unit that are too small to be visible at this scale, the occurrences are denoted 7
7 ) )
)
) Dease PzTrCClw
) ) )
) by outcrop location (x).
) ) ) ) Dease Lake Lake ) ) )
) ) ) ) !P ) ) ) !P ) ) Populated place (unclassified) ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! P
MinFile (labelled by MinFile number): Prospect, Showing, Anomaly ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! S ! E
Altered / mineralized rock samples ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !
Sample: fossil, isotopic dating method (U-Pb, Ar-Ar, Re-Os) labelled by preliminary date ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! *,F *,Z *,Ar *,Re Outcrop location ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !
Bedding: tops indicated, inclined, vertical, horizontal ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 6 ! % Î
Fabric: slaty cleavage or schistosity (inclined, vertical, second phase inclined, second phase vertical) ! ! ! ! ! ! ! ! ! ! ! ! Ï Ò Ð Ö
! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ø Fold axis: first phase, second phase Ö
Lineation: bedding/cleavage intersection, stretching lineation ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! F
Fabric: trachytic flow, brittle fracture/joint ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! qè qf Brittle shear: inclined, vertical ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! #
Dike: inclined, vertical ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! A B 0 0 0 0 0 0 ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! Â 0 0 Vein: inclined, vertical 7 7 3 3 4 4
DMO-6-49 6 6 0 0 ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 0 0 Geological contact: defined, approximate, inferred 0 0 0 0 7 7 ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 4 4 Inferred quaternary cover contact 6 6
Unconformity: defined, approximate, inferred ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ( (
DMO-33-284 JLO-28-287 Fault: defined, approximate, inferred ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !
JLO-28-285 ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ( ( ( ( ) )
Thrust fault: defined, approximate, inferred Axial trace of overturned regional fold: antiform, synform ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! I Z DMO-35-309
DMO-35-309Dup Contact metamorphic isograd: biotite in, cordierite in ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 7 7
Limit of mapping ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !
Roads: Highway 37, Telegraph Creek, Hluey Lake ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !(37 JLO-24-249 Elevation contours (20 m intervals): Major, Minor ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! JLO-24-244-2
! ! 0 0 0 Field stations (n = 955) 0 ! ! ! ! 0 0 0 2 0 6 6
* Map area = 1,275 km 4 ( ! 4 ( ! 6 6
0 Sample location (labelled by Sample Number) 0 0 0 0 0 ( ( 0 0
6 !
6 ! 4
4 ( ! ( !
6 56824.1 57025.4 57467.2 6
! !
! 1:100,000 ! 1:100,000 ( 56493.1 56931.3 57187.8 > 58624.5 ( BC Geological Survey Open File 2012-04 !LDI-19-164a 0 1 2 4 km ! 0 1 2 4 km Nanoteslas LDI-19-164b Geoscience BC Map 2012-08-1
! !
400000 410000 420000 430000 440000 400000 410000 420000 430000 440000 Dease Lake - References Altered / Mineralized Rock Samples (ICP-MS) Aeroquest Airborne (2012): Report on a helicopter-borne magnetic survey (Aeroquest job # 11-046) for Geoscience BC; Geoscience BC Report 2012-2, 11 pages. Data Sources SampleNumber UTM ZONE10 Unit LabNo Ag As Au Ba Bi Cd Ce Little Tuya River Geology Anderson, R.G. (1983): Geology of the Hotailuh batholith and surrounding volcanic and sedimentary rocks, north-central British Columbia; unpublished Ph.D. thesis, Carleton University, 669 pages. MinFile data Ash, C.H., Macdonald, R.W.J., Stinson, P.K., Fraser, T.M., Nelson, K.J., Arden, K.M. and Lefebure, D.V. (1997): Geology and mineral occurrences of the Tatogga Lake area; B.C. Ministry of Energy, Mines and Petroleum Resources, Open File 1997-3. Easting Northing Detection 0.1 1 2 1 0.1 0.1 1 MINFILE (2012): MINFILE BC mineral deposits database; B.C. Ministry of Energy Bamber, E. W. (2011): Report on two collections of upper Paleozoic invertebrate fossils from the Dease Lake area, northwestern British Columbia, NTS 104J-7, 104J-8; Geological Survey of Canada, Paleontological Report 01-EWB-2011, 3 pages. Units PPM PPM PPB PPM PPM PPM PPM and Mines, URL