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1
KORAB RESOURCES LIMITED
COMBINED
ANNUAL REPORT
EL 25136 and EL 25242
YEAR 2 Period Ending 11 September 2008
GREEN ALLIGATOR PROJECT
BATCHELOR
Northern Territory
By
John A Earthrowl MSc
for
KORAB RESOURCES LIMITED
KORAB HOUSE LEVEL 1, SUITE 6, 100 MILL POINT ROAD, SOUTH PERTH, 6151, WESTERN AUSTRALIA
PO BOX 195 SOUTH PERTH WA 6951 AUSTRALIA, Tel (08) 9474 6166 Fax (08) 9474 6266
www.korabresources.com.au
2
2
TABLE OF CONTENTS
SUMMARY
1 INTRODUCTION
2 TENEMENT STATUS
3 LOCATION
4 GEOLOGY
5 PREVIOUS EXPLORATION
6 EXPLORATION PROGRAM AND TARGETS
7 METHODS
7.1 Reconnaissance Ground Traversing
7.2 Mapping
7.3 Rock Chip Sampling
7.4 Ground Radiometrics
8 WORK DONE AND RESULTS
8.1 EL 25136
8.1.1 Geology
8.1.2 Radiometrics
8.1.3 Assay Results
8.2 EL 25242
8.2.1 Geology
8.2.2 Radiometrics
8.2.3 Assay Results
9 CONCLUSIONS
10 RECOMMENDATIONS
11 EXPENDITURE STATEMENT
11.1 EL 25136
11.2 EL 25242
12 NEXT YEARS PROGRAM AND BUDGET
3
3
LIST OF FIGURES
Fig 1 Location of ELs 25136 and 25242
Fig 2 ELs 25136, 25242 on Regional Geology Base map
Fig 3 EL 25136 Rock Chip Sample Locations
Fig 4 EL 25136 Ground Radiometric Readings
Fig 5 EL 25242 Rock Chip Sample Locations
Fig 6 EL 25242 Ground Radiometric Readings
APPENDICES
App 1A EL 25136 Spreadsheet: Rock Chip Samples
App 1B EL 25136 Spreadsheet : Radiometry
App 2A EL 25242 Spreadsheet : Rock Chip Samples
App 2B EL 25242 Spreadsheet : Radiometry
App 3 ELs 25136 / 25242 Assay Results of Rock Chip Samples
REFERENCES
Lally, J.H. (2002) Stratigraphy, structure and mineralization, Rum Jungle
Mineral Field, Northern Territory.
N.T.G.S. Record 2002-005
Mudrovska, I ( 2008) Korab Resources Ltd
Annual Report for EL 25136 and 25242
Unpublished / Closed File Report to DPIFM
4
4
SUMMARY
Field work on both tenements has successfully tested their stratigraphy and
upgraded their mineral potential.
One stratigraphic unit, the Mt Deane Volcanic Member, has returned
anomalous base metal and gold values that warrant follow up.
1 INTRODUCTION
This document is the Second Combined Annual Report for Exploration
Licences 25136 and 25242 covering the period 12 September 2007 to 11
September 2008.
These two tenements comprise part of Korab Resources Ltd.’s Green
Alligator Project in the Batchelor area of the Northern Territory, Australia.
2 TENEMENT STATUS
Both ELs 25136 and 25242 were granted 100% to Korab Resources Ltd. on
12 September 2006. EL 25136 consists of 3 subblocks totaling 1.59 km².
El 25242 consists of 4 subblocks totaling 1.96 km².
In view of the late start to field work, due to unavailability of experienced
exploration personnel, a waiver of reduction for both tenements was lodged
on 11 September 2008.
The tenements are planned to be transferred to Korab’s wholly owned
subsidiary Uranium Australia Ltd as explained in last years Annual Report.
3 LOCATION
ELs 25136 and 25242 are located approximately 80 kms south of Darwin,
contiguous to the Stuart Highway, just south of the Batchelor turnoff.
EL 25136’s centroid is at approximately 13º 2´ S, 131º 7´ E (WGS 84
729800E, 8558800N).
EL 25242’s centroid is at approximately 13º 4´ S, 131º 6´ E (WGS 84
728200E, 8555400N).
5
5
4 GEOLOGY
Both tenements fall within the Rum Jungle Uranium Field (RJUF) of the
Pine Creek Orogen and are underlain by the Early Proterozoic, Mount
Partridge and South Alligator stratgraphic Groups.
More specifically recent NTGS government mapping shows tenements to be
underlain by the following units as listed:
EL 25136 Ppw Wildman Siltstone
Ppa Acacia Gap Quartzite
Ppd Mount Deane Basic Volcanics
And EL 25242 Ppw Wildman Siltstone
Psg Gerowie Tuff
Psk Koolpin Formation
Mudrovska (2008) describes in considerable detail the distribution of various
metal prospects in the near vicinity of ELs 25136 and 25242.
5 PREVIOUS EXPLORATION
Both tenements have been covered by a number of exploration licences in
the past. In the 1970s and 1980s Uranerz Australia Ltd and Minad had a
joint venture in the area. Their target was uranium mineralization as known
at Whites / Dysons in the Embayment Area of the RJUF.
As the area of ELs 25136 and 25242 did not include either the Coomalie
Dolomite or Whites Formation, no detailed work was done on the ground as
they were the only stratigraphy targeted in that era.
More regional exploration by other companies has been described in
Mudrovska (2008).
6
6
6 EXPLORATION PROGRAM AND TARGETS
The RJUF is prospective for the following commodities: uranium, copper,
cobalt, nickel, lead, silver, gold, phosphate, magnesium and
platinum/palladium.
With these tenements Korab Resources is testing relatively unexplored
ground and therefore will examine the tenements with an open mind.
In the case of uranium the exploration methods used will cover the
possibilities of Vein–Type uranium mineralization being present, as is
known south of Adelaide River township.
7 METHODS
With no known previous detailed exploration results from the area of ELs
25136 and 25242, Korab’s field work has consisted of regional traversing
for familiarisation with the stratigraphy and checking government mapping,
the collection of rock chip samples from all stratigraphic units and the
recording of detailed radiometrics across the various stratigraphic units.
7.1 RECONNAISSANCE GROUND TRAVERSING
On each EL ground traverse routes were chosen on the basis of access
and to cut across the stratigraphy. Manmade features such as tracks
and fence lines and natural features such as creek beds were chosen.
On each tenement it was possible to sample all mapped stratigraphic
units present.
7.2 MAPPING
As mentioned in Section 4 current government mapping has
delineated, by interpretation, certain stratigraphic units to be present
on each of the tenements. It is known that certain aspects of the
stratigraphy of the RJUF remain undefined and not well understood.
The stratigraphic nomenclature has been under continuous review
since the early 1970s.
7
7
One stratigraphic unit that has been identified in various places and at
various levels in the stratigraphy is the Mout Deane Volcanic Member
of the Wildman Siltstone Formation in the Mount Partridge Group.
The Mt .Deane Volcanics are described as “Altered basic volcanics, in
places vesicular or brecciated” (Lally 2003). This unit is the only
known basic extrusive rock in the RJUF. The only other basic rock is
the intrusive Zamu Dolerite.
EL 25136 is shown to be underlain by a bed of Mt Deane Volcanics
extending the full length of the tenement. Older maps had shown
isolated, discontinuous outcrops.
EL 25242 has the Mt Deane Volcanics present to the northeast and to
the west but not within the tenement.
7.3 ROCK CHIP SAMPLING
Rock chip samples were collected on the reconnaissance traverses
whenever a different stratigraphic unit or gossanous material was
encountered.
Their locations were GPS recorded, the lithology described, a sample
number assigned and a 1-2 kg sample submitted for assay.
7.4 GROUND RADIOMETRICS
Total count scintillometer readings were taken at approximately 20
metre intervals along all traverses.
If on an EW or NS traverse, control was by maintaining the GPS
reading.On an irregular traverse along a creek or fenceline readings
were taken at approximately paced intervals of 20m.and the GPS
reading recorded.
Total count radiometrics were taken with an SAIG Exploranium GR -
110-G scintillometer. Readings were taken with the instrument on the
ground and after an averaged 10 second accumulation.
8
8
7.5 ASSAYING
All rock samples were submitted to the Darwin based laboratory,
Northern Territory Environmental Laboratories (NTEL). Assay
methods and detection limits were chosen commensurate with the
grades expected.
Samples were routinely analysed for Cu, Co, Ni, Pb, Zn, U and Au.
8 WORK DONE AND RESULTS
8.1 EL 25136
The following field work was done on this tenement in Year 2 as
shown on Fig 3 and Fig 4 and listed in the appendices :
3.04 kms of foot traversing by geologist and field assistant
9 Rock samples collected (#s 110681 to 110689 )
152 Scintillometer readings taken
The traverse routes were chosen to cut across all the stratigraphic
units as shown to be present on the tenement by available modern
government mapping.
The northeastern traverse followed a power line paralleling the Stuart
Highway. The east-west traverse was chosen to go over the main hill
at right angles to strike on WGS84 8559900 Northing. The sinuous
traverse near the middle of the tenement followed an incised creek
course.
8.1.1 Geology
Geological observations on the traverse show the resistant Ppa
Acacia Gap Quartzite to be present as ridge forming but on the
1:100,000 NTGS map is plotted approximately 100m too far
west.
The Mt Deane Volcanics were found to be present west of
where mapped (Samples 110682/683) but also at a second level
west of the Acacia Gap Tongue Quartzite (Sample
110688/689).
9
9
8.1.2 Radiometrics
Appendix 1B lists the radiometric readings from the traverses.
The three different traverses’ radiometrics can be summarised :
Total Readings Maximum Minimum Average
Power Line Traverse 64 238 c/s 101c/s 188 c/s
East -West Traverse 22 235 c/s 96 c/s 144 c/s
Creek Traverse 58 251 c/s 61 c/s 164 c/s
The low readings around 100 c/s correlate well with the
quartzite.
No significant anomalous radiometric readings were obtained
on this year’s traversing.
8.1.3 Assay Results
Assay results for EL 25136 are shown in Appendix 3.
Samples 110681 to 110689 were collected from the three
traverses and their location is shown on Fig 3.
Assay results from the nine samples can be summarized as
follows:
Element Range Maximum Sample No
Au 1-43 ppb 43 ppb 110682
Co 1-281 ppm 281 ppm 110682
Cu 5- 195 ppm 195 ppm 110683
Ni 10- 1730 ppm 1730 ppm 110682
Pb 2-20 ppm 20 ppm 110682
U less than DL
Zn 10-990 ppm 990 ppm 110682
As can be seen all maxima came from Sample Nos 110682 or
110683.
10
10
Appendix 1A shows these samples to be Mt Deane Volcanics.
The most significant value is the 0.1730% Ni.
(As a result of these assays an additional 11 samples have been
collected in the vicinity of 110682. These were collected on 17
September 2008 after the tenements’ anniversary. They are
nevertheless recorded in App 1A and shown in Fig 3. Their
assays will be shown in next year’s Annual report.)
8.2 EL 25242
The following field work has been done on this tenement during this
year as shown on Figs 5 and 6 and listed in Appendix 2A and 2B:
3.62 kms of foot traversing by geologist and field assistant
22 Rock Samples collected (#s 110659 to 110680)
181 Scintillometer readings taken
8.2.1 Geology
The route of the foot traverse followed the fence line of the
railway corridor.
This conveniently transected all of the stratigraphic units
interpreted to be present on the tenement viz. from south to
north ….Psg Gerowie Tuff, Psk Koolpin Formation, Ppw
Wildman Siltstone, Ppa Acacia Gap Quartzite.
In the field a wide variety of rock types were encountered as per
App 2A, and on this first reconnaissance traverse the contacts
between the NTGS mapped stratigraphic units could not be
recognised.
One discrepancy however was the presence of Mt Deane
Volcanics, Ppd, at sample site 110669 suggesting that unit
continues into the EL from the north or west.
11
11
8.2.2 Radiometrics
The rail corridor traverse comprised 181 readings with a
maximum of 376 c/s, a minimum of 123 c/s and an average of
251 c/s.
Grouping these data on the basis of NTGS interpreted geology
we get :
No.Readings Maxima Minima Average
Gerowie Tuff 62 309 c/s 217 c/s 258 c/s
Koolpin 36 319 176 268
Wildman Siltstone 57 323 123 229
(Another 26 readings were from the rail cutting detail. See map)
These data do not clearly show any marked difference in
radiometrics for the different units. This may be the case or
their groupings may be in error as stratigraphic units could not
be differentiated in the field.
One reading of 700 c/s from Sample 110679 (GPS 728355E,
8556218N) from the cutting wall was on an outcrop of
gossanous quartzite.
8.2.3 Assay Results
Appendix 3, sample numbers 110659 to 110680, are results of
analysis of the 22 rock samples collected from EL 25242.
These results can be summarized as follows:
Element Range Maxima Sample No.
Au 1-33 ppb 33 ppb 110666
Co 1-100 ppm 100 ppm 110669
Cu 5-255 ppm 255 ppm 110666
Ni 5-610 ppm 610 ppm 110668
Pb 4-130 ppm 130 ppm 110666
U 5-20 ppm 20 ppm 110679/80
Zn 10-1070 ppm 1070 ppm 110668
12
12
Sample 110666 was of rubble of “iron rich
Sediments/Volcanics”…probably Koolpin. The highs of 255
Cu, 130 Pb are moderately anomalous. The gold of 33 ppb will
need following up.
Sample 110669 was of “deeply wthrd choc.brown , massive,
unlaminated basic volcanic – probably Mt Deane volcanics. 100
Co is moderately anomalous.
Sample 110668 was of “siltstone, ferruginous, laminated
“..probably Koolpin Formation. The 610Ni and 1070Zn are
both moderately anomalous.
Samples 110679 and 110680 were both of “Quartzite, pyritic,
carbonaceous” probably Acacia Gap Quartzite. This had given
a 700 c/s TC reading. The assay value of 20 ppm U does not
explain the 700 c/s.
This will need field checking.
9. CONCLUSIONS
The year’s field work has given a good regional overview of the mineral
potential of the two tenements.
The reconnaissance geological mapping has indicated most NTGS
interpreted geological units to be present albeit in places misplaced by up to
100m.
In the case of the Mt Deane Volcanic Member, its distribution is not yet well
defined and Korab’s traversing indicates this unit may well be present at
more than one stratigraphic level.
Radiometric traversing of TC (gamma) has shown no clear relationship with
different stratigraphic units as mapped.
Except for one reading of 700 c/s no obviously anomalous readings have
been recorded.
13
13
Several anomalous assay values were obtained and will need following up,
such as:
On EL 25136 Samples 110682 and 110683 of Mt Deane Volcanics
have returned anomalous assay values in Ni, Co, Zn and gold.
There is no record of the Mt Deane Volcanics having been intersected
in drilling by either government or exploration companies in the past.
Sample 110668 from EL 25242 returned anomalous value in Ni and
Zn from a sample of Koolpin Formation.
The high radiometric reading of 700 c/s from the Acacia Gap
Quartzite which assayed 20 ppm U needs further followup.
10 RECOMMENDATIONS
Further work is warranted on both tenements.
Korab Resources request for a waiver of reduction was justified and
warranted in the light of the company not being able to find suitable field
geologists to do the work until late in this year.
The now recognized potential of the hitherto previously untested Mt Deane
Volcanic Member clearly needs follow up.
An additional 10 samples have already been collected from the environs of
the discovery 0.173% Ni site. Additional geology mapping to delineate this
unit in both tenements is highly recommended. In addition to nickel, the Mt
Deane Volcanics show cobalt, copper and gold anomalism. The indicated
basic petrology of the Mt Deane unit would also suggest potential for
platinum, palladium and rhodium.
Specific recommendations for EL 23516 are as follows :
Further east-west traversing of the narrow EL to establish the position
and any continuity of the Mt Deane volcanics.
Further north-south traversing to follow the Mt Deane volcanics and
to locate that unit’s maximum thickness for drilling.
Get good structural information on the Mt Deane Volcanics in order
to locate the optimum site for a drill hole to intersect a thick part of
the unit below the water table.
Further sampling of the Mt Deane Volcanics to define the distribution
of metals vertically and laterally.
14
14
Further test other stratigraphy with rock sampling and radiometrics.
Investigate availability of indirect mapping techniques that would
assist with the above (Hymap? etc)
Specific recommendations for EL 25242 are as follows:
Trace the Mt Deane Volcanics from the northeast and west where
already mapped by NTGS, into EL 25242.
As per EL 25136 re Mt Deane Volcanic Member.
Further test other stratigraphy with sampling and radiometrics.
11. EXPENDITURE STATEMENT
(Yet to be supplied by Korab Perth office )
12. NEXT YEARS PROGRAM
The Year 3 program for each tenement is based on the recommendations as
specified above.
It is estimated the expenditure on EL 25136 will be $5,200.00
It is estimated the expenditure on EL 25242 will be $5,300.00
15
15
Figure 1: Location of ELs 25136 and 25242
16
16
Figure 2: Geological setting of the Batchelor and Green Alligator projects showing
location of ELs 25136 and 25242
17
17
Figure 3: EL 25136 Rock Chip Sample Locations
18
18
Figure 4: EL 24136 Radiometrics
19
19
Figure 5: EL 25242 Rock Chip Sample Locations
20
20
Figure 6: EL 25242 Radiometrics on Geology Base
21
21
Appendix 1A
Ten
emen
tUT
M
WG
S 8
4
WG
S 8
4
Sam
ple
Sam
ple
S
amp
le L
ITH
OL
OG
Y
Z
on
e E
AS
T
NO
RT
H
Nu
mb
er T
yp
e
Date
EL
25
13
6 5
2 L
7
300
02
85
60
40
0 W
F 1
10
68
1
Ou
tcrop
, com
po
site 11/0
8/2
008
Q
tzite,dark
grey
,py
ritic,carbo
nn
aceou
s,Acacia G
ap T
ong
ue M
ember
EL
25
13
6 5
2 L
7
301
16
85
60
26
8 W
F 1
10
68
2
Ou
tcrop
, com
po
site 11
/08
/200
8
Deep
ly w
thrd
basic v
olcan
ic.Mt D
eane V
olc.
EL
25
13
6 5
2 L
7
300
85
85
60
03
6 W
F 1
10
68
3
Ou
tcrop
, com
po
site 11/0
8/2
008
D
eeply
wth
rd,flo
w b
and
ed v
esicular b
asalt.Mt D
eane V
olcs
EL
25
13
6 5
2 L
7
300
43
85
59
80
1 W
F 1
10
68
4
Ou
tcrop
, com
po
site 11
/08
/200
8
Qtzite g
rey an
d S
chist,sericitic.
EL
25
13
6 5
2 L
7
298
44
85
59
90
4 W
F 1
10
68
5
Ou
tcrop
, com
po
site 11/0
8/2
008
Q
tzite,grey
,py
ritic.Av
cacia Gap
To
ngu
e Mem
ber
EL
25
13
6 5
2 L
7
296
70
85
59
90
0 W
F 1
10
68
6
Su
bo
utcro
p,co
mp
osie 1
1/0
8/2
00
8
Qtzite,g
rey,p
yritic..
EL
25
13
6 5
2 L
7
296
92
85
58
97
6 W
F 1
10
68
7
Ou
tcrop
, com
po
site 11/0
8/2
008
Q
tzite,grey
,py
ritic
EL
25
13
6 5
2 L
7
296
25
85
58
62
0 W
F 1
10
68
8
Ru
bble,co
mp
osite 1
1/0
8/2
008
W
thrd
dark
bro
wn
vo
lcanic.in
terbed
s Qtzite. M
t Dean
e Vo
lc.
EL
25
13
6 5
2 L
7
295
43
85
58
34
0 W
F 1
10
68
9
Ru
bble,co
mp
osite 1
1/0
8/2
008
M
t Dean
e Vo
lc Mem
ber.
EL
25
13
6 5
2 L
7
301
19
85
60
25
4 W
F 1
10
69
0
Ou
tcrop
,com
po
site 17/0
9/2
008
V
ery,w
eathered
Mt D
eane V
olcan
ic Mem
ber,B
otto
m
EL
25
13
6 5
2 L
7
301
06
85
60
25
4 W
F 1
10
69
1
Ou
tcrop
,com
po
site 17/0
9/2
008
V
ery,w
eathered
Mt D
eane V
olcan
ic Mem
ber,M
idd
le
EL
25
13
6 5
2 L
7
300
79
85
60
25
8 W
F 1
10
69
2
Ou
tcrop
,com
po
site 17/0
9/2
008
V
ery,w
eathered
Mt D
eane V
olcan
ic Mem
ber,T
op
EL
25
13
6 5
2 L
7
300
77
85
60
20
6 W
F 1
10
69
3
Ou
tcrop
,com
po
site 17/0
9/2
008
V
ery,w
eathered
Mt D
eane V
olcan
ic Mem
ber,T
op
EL
25
13
6 5
2 L
7
300
92
85
60
20
0 W
F 1
10
69
4
Ou
tcrop
,com
po
site 17/0
9/2
008
V
ery,w
eathered
Mt D
eane V
olcan
ic Mem
ber,M
idd
le
EL
25
13
6 5
2 L
7
300
98
85
60
19
8 W
F 1
10
69
5
Ou
tcrop
,com
po
site 17/0
9/2
008
V
ery,w
eathered
Mt D
eane V
olcan
ic Mem
ber,B
otto
m
EL
25
13
6 5
2 L
7
300
83
85
60
10
6 W
F 1
10
69
6
Ou
tcrop
,com
po
site 17/0
9/2
008
V
ery,w
eathered
Mt D
eane V
olcan
ic Mem
ber,B
otto
m
EL
25
13
6 5
2 L
7
300
80
85
60
10
2 W
F 1
10
69
7
Ou
tcrop
,com
po
site 17/0
9/2
008
V
ery,w
eathered
Mt D
eane V
olcan
ic Mem
ber,M
idd
le
EL
25
13
6 5
2 L
7
300
77
85
60
10
6 W
F 1
10
69
8
Ou
tcrop
,com
po
site 17/0
9/2
008
V
ery,w
eathered
Mt D
eane V
olcan
ic Mem
ber,M
Idd
le
EL
25
13
6 5
2 L
7
300
75
85
60
11
2 W
F 1
10
69
9
Ou
tcrop
,com
po
site 17/0
9/2
008
V
ery,w
eathered
Mt D
eane V
olcan
ic Mem
ber,M
Idd
le
EL
25
13
6 5
2 L
7
300
71
85
60
11
2 W
F 1
10
70
0
Ou
tcrop
,com
po
site 17/0
9/2
008
V
ery,w
eathered
Mt D
eane V
olcan
ic Mem
ber,T
op
22
22
Appendix 1B
Creek Bed Traverse 12-Aug-08
730044 8558996 170
730027 8558998 186
730008 8558996 181
729987 8558998 174
729973 8558998 156
729956 8558992 143
729938 8558984 126
729928 8558992 151
729907 8558992 116
729889 8558992 105
729873 8558989 73
729867 8558986 86
729855 8558990 75
729817 8558964 61 Qtzite O/C
729812 8558974 109
729806 8558978 147
729786 8558982 246
729765 8558982 236
729750 8558980 251
729734 8558976 239
729722 8558964 220
729708 8558954 229
729704 8558936 214
729704 8558916 219
729697 8558900 232
729683 8558988 222
729669 8558882 215
729665 8558862 212
729658 8558844 193
729651 8558826 194
729651 8558806 193
729652 8558794 199
729650 8558776 186
729646 8558752 204
729643 8558734 190
729640 8558714 192
729636 8558696 197
729632 8558682 201
729633 8558662 187
729630 8558642 175
729627 8558624 188
729618 8558608 134
729612 8558590 114
729610 8558576 140
729607 8558560 126
729603 8558544 121
23
23
729600 8558528 118
729596 8558510 141
729595 8558494 142
729587 8558478 143
729577 8558464 119
729575 8558446 125
729568 8558426 127
729561 8558410 153
729555 8558394 112
729549 8558376 131
729545 8558362 147
729542 8558326 170 End of Creek traverse.
East West Traverse on 8559900N
730050 8559900 135
730030 8559900 141
730010 8559900 125
729990 8559900 158
729970 8559900 136
729950 8559900 137
729930 8559900 235
729910 8559900 124
729890 8559900 97
729870 8559900 115
729850 8559900 96
729830 8559900 129
729810 8559900 136
729790 8559900 129
729770 8559900 152
729750 8559900 137
729730 8559900 110
729710 8559900 129
729690 8559900 141
729670 8559900 169
729650 8559900 225
729630 8559900 212 End of EW Traverse
Creek Bed Traverse 12-Aug-08
730044 8558996 170
730027 8558998 186
730008 8558996 181
729987 8558998 174
729973 8558998 156
729956 8558992 143
729938 8558984 126
729928 8558992 151
24
24
729907 8558992 116
729889 8558992 105
729873 8558989 73
729867 8558986 86
729855 8558990 75
729817 8558964 61 Qtzite O/C
729812 8558974 109
729806 8558978 147
729786 8558982 246
729765 8558982 236
729750 8558980 251
729734 8558976 239
729722 8558964 220
729708 8558954 229
729704 8558936 214
729704 8558916 219
729697 8558900 232
729683 8558988 222
729669 8558882 215
729665 8558862 212
729658 8558844 193
729651 8558826 194
729651 8558806 193
729652 8558794 199
729650 8558776 186
729646 8558752 204
729643 8558734 190
729640 8558714 192
729636 8558696 197
729632 8558682 201
729633 8558662 187
729630 8558642 175
729627 8558624 188
729618 8558608 134
729612 8558590 114
729610 8558576 140
729607 8558560 126
729603 8558544 121
729600 8558528 118
729596 8558510 141
729595 8558494 142
729587 8558478 143
729577 8558464 119
729575 8558446 125
729568 8558426 127
729561 8558410 153
729555 8558394 112
729549 8558376 131
729545 8558362 147
729542 8558326 170 End of Creek traverse.
25
25
Appendix 2A
SA
MP
LE
S
Te
nem
ent
UT
M
WG
S 8
4
WG
S 8
4
Sam
ple
S
am
ple
S
am
ple
d
Sam
ple
LIT
HO
LO
GY
S
TR
UC
TU
RE
Z
one
EA
ST
N
OR
TH
N
um
be
r T
ype
By
Date
EL 2
5242
52 L
728198
8554886
W
F 1
10659
Outc
rop, c
om
posite
JA
E
7/0
8/2
008
B
reccia
, cata
cla
stic
, with
Fe
irridescent m
atrix
EL 2
5242
52 L
728365
8556218
W
F 1
10660
Outc
rop, c
om
posite
JA
E
7/0
8/2
008
C
hert/S
iltsto
ne, s
ulp
hid
e s
tain
ed.
EL 2
5242
52 L
728154
8554700
W
F 1
10661
Rubble
JA
E
9/0
8/2
008
S
hale
,hem
atite
-seric
ite
EL 2
5242
52 L
728166
8554750
W
F 1
10662
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
C
hert,d
k g
rey,S
iltst.lt b
row
n,in
terb
eds
Strik
e 0
50 M
,Dip
85 E
EL 2
5242
52 L
728170
8554800
W
F 1
10663
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
C
hert,la
min
ate
d,g
rey-g
reen.V
olc
? G
ero
wie
Tu
ff
EL 2
5242
52 L
728176
8554850
W
F 1
10664
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
S
iltst./S
hale
, seric
itic,F
e s
tain
ed,b
uff c
lrd.
Strik
e 0
87 M
, Dip
85 S
EL 2
5242
52 L
728184
8554900
W
F 1
10665
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
S
hale
/Silts
t.lam
inate
d,h
ighly
conto
rted
S
trike 0
40 M
,Dip
40 E
EL 2
5242
52 L
728190
8554950
W
F 1
10666
Rubble
,com
posite
JA
E
9/0
8/2
008
Iro
n ric
h S
edim
ents
/Volc
anic
s. U
ndif.?
?
EL 2
5242
52 L
728196
8555000
W
F 1
10667
Rubble
, cuttin
g
JA
E
9/0
8/2
008
S
iltst,w
ith q
tz v
ein
ing.B
uff c
olrd
S
trike 1
00 M
, Dip
30 S
EL 2
5242
52 L
728270
8555525
W
F 1
10668
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
S
iltst.fe
rrug.la
min
ate
d
Strik
e 0
58 M
,Dip
60 S
EL 2
5242
52 L
728280
8555575
W
F 1
10669
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
D
eeply
wth
rd.c
hoc b
row
n m
assiv
e,u
nla
m.B
asic
Volc
s.M
t Deane V
olc
Join
ts 1
60 M
,Dip
60 W
EL 2
5242
52 L
728280
8556525
W
F 1
10670
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
S
iltst./C
hert in
terb
eds,w
ell la
min
ate
d,c
ream
-yello
w.G
ero
wie
Tu
ff?
Strik
e 0
40 M
,Dip
64 S
EL 2
5242
52 L
728354
8556150
W
F 1
10671
Suboutc
rop,c
om
posite
JA
E
9/0
8/2
008
Late
ritised S
hale
,deeply
wth
rd.
EL 2
5242
52 L
728362
8556200
W
F 1
10672
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
In
terb
edded P
hyllite
,narrio
w Q
tz V
ein
s,p
yritic
.Very
fold
ed.
Strik
e 0
20 M
,Dip
20 W
EL 2
5242
52 L
728361
8556250
W
F 1
10673
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
Q
tzite
.carb
onnaceous-p
yritic
.Gossanous w
ith s
ulp
hur?
S
trike 1
10 M
,Dip
62 S
EL 2
5242
52 L
728361
8556300
W
F 1
10674
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
In
terb
edded F
e ric
h S
iltst.a
nd p
yritic
chert?
S
trike 0
95 M
,Dip
64 S
EL 2
5242
52 L
728384
8556350
W
F 1
10675
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
In
terb
edded P
hyllite
,seric
itic a
nd p
yritic
Qtz
ite,d
rk g
rey.
Strik
e 0
80 M
,Dip
70 S
EL 2
5242
52 L
728402
8556400
W
F 1
10676
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
V
aria
ble
Schis
t/Sh/P
hyllite
,seric
itic,lt b
row
n
Strik
e 0
70 M
,Dip
60 S
EL 2
5242
52 L
728397
8556450
W
F 1
10677
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
Q
tzite
,dark
gre
y,p
yritic
.Acacia
Gap T
ongue M
em
ber?
EL 2
5242
52 L
728406
8556500
W
F 1
10678
Outc
rop,c
uttin
g
JA
E
9/0
8/2
008
Q
tzite
,dark
gre
y w
ith p
yritic
cla
sts
?
Strik
e 0
30 M
,Dip
35 E
EL 2
5242
52 L
728350
8556220
W
F 1
10679
Outc
rop,c
.West s
ide
JA
E
9/0
8/2
008
Q
tzite
.pyritic
,carb
onnaceous.
EL 2
5242
52 L
728368
8556214
W
F 1
10680
Outc
rop,c
u.E
ast s
ide
JA
E
9/0
8/2
008
Q
tzite
.pyritic
,carb
onnaceous.S
am
e u
nit a
s 1
10679.
26
26
Appendix 2B
RADIOMETRICS
Railway Traverse 11-08-08
Tenement UTM WGS 84 WGS 84 Scintillometer xx=Highs Comments
Zone EAST NORTH Reading LL=Lows
On Ground
10 sec
Average
counts/sec
EL 25242 52 L 727787 8553600 281
EL 25242 52 L 727795 8553618 232
EL 25242 52 L 727803 8553636 288
EL 25242 52 L 727812 8553658 283
EL 25242 52 L 727818 8553674 272
EL 25242 52 L 727822 8553690 275
EL 25242 52 L 727830 8553710 267
EL 25242 52 L 727836 855373 266
EL 25242 52 L 72784 8553750 270
EL 25242 52 L 727850 8553766 259
EL 25242 52 L 727859 8553784 255
EL 25242 52 L 727863 8553802 251
EL 25242 52 L 727871 8553818 260
EL 25242 52 L 727880 8553836 243
EL 25242 52 L 727886 8553854 272
EL 25242 52 L 727893 8553874 270
EL 25242 52 L 727900 8553892 270
EL 25242 52 L 727906 8553910 265
EL 25242 52 L 727912 8553926 262
EL 25242 52 L 727918 8553946 237
EL 25242 52 L 727924 8553964 245
EL 25242 52 L 727930 8553982 232
EL 25242 52 L 727936 8554004 264
EL 25242 52 L 727944 8554014 217
EL 25242 52 L 727950 8554036 230
EL 25242 52 L 727956 8554056 226
EL 25242 52 L 727963 8554072 236
EL 25242 52 L 727968 8554094 230
EL 25242 52 L 727977 8554110 232
EL 25242 52 L 727982 8554128 232
EL 25242 52 L 727986 8554146 236
EL 25242 52 L 727992 8554164 231
EL 25242 52 L 727998 8554182 238
EL 25242 52 L 728003 8554200 264
EL 25242 52 L 728009 8554218 250
EL 25242 52 L 728015 8554234 259
EL 25242 52 L 728026 8554252 241
EL 25242 52 L 728032 8554268 278
EL 25242 52 L 728038 8554286 305 xx
27
27
EL 25242 52 L 728044 8554302 294
EL 25242 52 L 728050 8554320 309 xx
EL 25242 52 L 728056 8554338 242
EL 25242 52 L 728062 8554356 245
EL 25242 52 L 728068 8554372 277
EL 25242 52 L 728074 8554390 285
EL 25242 52 L 728080 8554410 243
EL 25242 52 L 728028 8554428 285
EL 25242 52 L 728094 8554446 273
EL 25242 52 L 728100 8554464 263
EL 25242 52 L 728106 8554480 232
EL 25242 52 L 728114 8554498 225
EL 25242 52 L 728120 8554514 235
EL 25242 52 L 728126 8554528 276
EL 25242 52 L 728130 8554548 274
EL 25242 52 L 728135 8554566 244
EL 25242 52 L 728139 8554584 243
EL 25242 52 L 728143 8554604 246
EL 25242 52 L 728146 8554624 256
EL 25242 52 L 728150 8554642 271 x
EL 25242 52 L 728156 8554660 285 x
EL 25242 52 L 728159 8554678 296 x
EL 25242 52 L 728166 8554698 303 xx
217
EL 25242 52 L 728170 8554714 308 xx Needs
EL 25242 52 L 728173 8554730 298 x field
EL 25242 52 L 728176 8554748 281 x checking
EL 25242 52 L 728178 8554766 319 xx
EL 25242 52 L 728180 8554784 261 x
EL 25242 52 L 728183 8554804 305 xx
EL 25242 52 L 728186 8554824 310 xx
EL 25242 52 L 728188 8554844 255 x
EL 25242 52 L 728191 8554864 181 LL
EL 25242 52 L 728195 8554884 176 LL
EL 25242 52 L 728198 8554904 226 x
EL 25242 52 L 728200 8554920 209 x
EL 25242 52 L 728202 8554936 255 x
EL 25242 52 L 728203 8554954 314 xx
EL 25242 52 L 728203 8554974 317 xx
EL 25242 52 L 728203 8554992 309 xx
EL 25242 52 L 728210 8555012 261
EL 25242 52 L 728211 8555028 236
EL 25242 52 L 728214 8555044 243
EL 25242 52 L 728219 8555064 260
EL 25242 52 L 728221 8555084 259
EL 25242 52 L 728224 8555104 272
EL 25242 52 L 728225 8555122 288
EL 25242 52 L 728229 8555138 244
EL 25242 52 L 728232 8555158 257
EL 25242 52 L 728235 8555178 271
28
28
EL 25242 52 L 728238 8555196 237
EL 25242 52 L 728241 8555216 240
EL 25242 52 L 728243 8555236 234
EL 25242 52 L 728246 8555254 276
EL 25242 52 L 728247 8555272 281
EL 25242 52 L 728251 8555290 306 xx
EL 25242 52 L 728252 8555310 292
EL 25242 52 L 728255 8555330 294
EL 25242 52 L 728257 8555348 319 xx
EL 25242 52 L 728260 8555366 270
176
EL 25242 52 L 728265 8555386 240
EL 25242 52 L 728266 8555404 244
EL 25242 52 L 728269 8555422 239
EL 25242 52 L 728271 8555440 228
EL 25242 52 L 728273 8555458 220
EL 25242 52 L 728274 8555478 212
EL 25242 52 L 728277 8555498 211
EL 25242 52 L 728281 8555518 208
EL 25242 52 L 728281 8555538 186 LL
EL 25242 52 L 728282 8555556 145 LL
EL 25242 52 L 728284 8555574 123 LL
EL 25242 52 L 728289 855592 131 LL
EL 25242 52 L 728290 8555612 153 LL
EL 25242 52 L 728292 8555630 162 LL
EL 25242 52 L 728295 8555648 190 LL
EL 25242 52 L 728298 8555666 195 LL
EL 25242 52 L 728303 8555684 199 LL
EL 25242 52 L 728307 8555700 225
EL 25242 52 L 728312 8555716 239
EL 25242 52 L 728314 8555734 254
EL 25242 52 L 728315 8555752 265
EL 25242 52 L 728318 8555772 223
EL 25242 52 L 728320 8555792 240
EL 25242 52 L 728323 8555810 228
EL 25242 52 L 728326 8555830 228
EL 25242 52 L 728328 8555850 251
EL 25242 52 L 728331 8555868 223
EL 25242 52 L 728334 8555886 211
EL 25242 52 L 728337 8555906 217
EL 25242 52 L 728339 8555926 229
EL 25242 52 L 728340 8555944 247
EL 25242 52 L 728344 8555962 229
EL 25242 52 L 728347 8555980 235
EL 25242 52 L 728348 8556000 232
EL 25242 52 L 728351 8556020 231
EL 25242 52 L 728355 8556038 246
EL 25242 52 L 728356 8556058 247
EL 25242 52 L 728359 8556078 239
EL 25242 52 L 728361 8556098 237
29
29
EL 25242 52 L 728358 8556118 252
EL 25242 52 L 728349 8556134 229
EL 25242 52 L 728353 8556154 232
EL 25242 52 L 728359 8556172 261
EL 25242 52 L 728362 8556190 268
EL 25242 52 L 728365 8556208 292
EL 25242 52 L 728369 8556228 313 xx
EL 25242 52 L 728370 8556246 323 xx
EL 25242 52 L 728371 8556266 303 xx
EL 25242 52 L 728376 8556286 308 xx
EL 25242 52 L 728378 8556304 252
EL 25242 52 L 728382 8556322 261
EL 25242 52 L 728382 8556340 276
EL 25242 52 L 728384 8556360 210
EL 25242 52 L 728387 8556380 231
EL 25242 52 L 728393 8556394 209
EL 25242 52 L 728402 8556406 222
EL 25242 52 L 728393 8556428 173 LL
123
EL 25242 52 L 728401 8556440 244
EL 25242 52 L 728395 8556456 196 LL
EL 25242 52 L 728398 8556472 214
EL 25242 52 L 728400 8556492 223
EL 25242 52 L 728404 8556500 247
EL 25242 52 L 728394 8556500 193 LL
EL 25242 52 L 728392 8556482 222
EL 25242 52 L 728391 8556462 250
EL 25242 52 L 728386 8556444 243
EL 25242 52 L 728384 8556424 184 LL
EL 25242 52 L 728375 8556410 123 LL
EL 25242 52 L 728374 8556396 210
EL 25242 52 L 728377 8556378 226
EL 25242 52 L 728375 8556360 236
EL 25242 52 L 728376 8556342 239
EL 25242 52 L 728379 8556324 259
EL 25242 52 L 728367 8556306 252
EL 25242 52 L 728366 8556292 335 xxx
EL 25242 52 L 728365 8556276 312 xx
EL 25242 52 L 728361 8556258 376 xxxx
EL 25242 52 L 728359 8556238 329 xx
EL 25242 52 L 728356 8556220 330 xx
EL 25242 52 L 728354 8556204 312 xx
EL 25242 52 L 728350 8556184 270
EL 25242 52 L 728347 8556168 299
EL 25242 52 L 728347 8556148 302 xx
249.5054348
EL 25242 52 L 728355 8556218 700 In cutting wall
46158.50543
30
30
Appendix 3
IDENT Job no Project code Au Au_R Au_R Co Cu Ni Pb U Zn
UNITS ppb ppb ppb ppm ppm ppm ppm ppm ppm
SCHEME FA25_MS FA25_MS FA25_MS G421M G421M G421M G421M G421M G421M
110659 EL11570 110659-110689 1 -- -- <1 30 <5 14 <5 10
110660 EL11570 110659-110689 <1 -- -- <1 <5 15 12 <5 30
110661 EL11570 110659-110689 2 -- -- 7 45 30 40 10 20
110662 EL11570 110659-110689 <1 -- -- 2 10 10 6 <5 20
110663 EL11570 110659-110689 2 -- -- 34 145 80 10 10 230
110664 EL11570 110659-110689 6 -- -- 2 40 10 28 10 10
110665 EL11570 110659-110689 10 12 -- 2 55 20 38 5 20
110666 EL11570 110659-110689 32 33 -- 12 255 50 130 10 20
110667 EL11570 110659-110689 4 -- -- 16 190 95 32 5 120
110668 EL11570 110659-110689 3 -- -- 60 60 610 42 10 1070
110669 EL11570 110659-110689 <1 -- -- 100 120 385 20 <5 450
110670 EL11570 110659-110689 2 -- -- 18 20 115 26 <5 350
110671 EL11570 110659-110689 <1 -- -- 3 10 25 24 <5 60
110672 EL11570 110659-110689 <1 -- -- 3 20 25 16 <5 60
110673 EL11570 110659-110689 4 -- -- 1 <5 15 22 <5 30
110674 EL11570 110659-110689 <1 -- -- 2 15 25 14 <5 30
110675 EL11570 110659-110689 3 -- -- 2 10 15 4 <5 10
110676 EL11570 110659-110689 2 -- -- <1 25 10 16 <5 10
110677 EL11570 110659-110689 <1 -- -- 1 <5 5 4 <5 10
110678 EL11570 110659-110689 <1 -- -- <1 10 5 6 <5 <10
110679 EL11570 110659-110689 3 -- -- <1 5 10 52 20 120
110680 EL11570 110659-110689 3 -- -- <1 <5 5 56 20 60
110681 EL11570 110659-110689 <1 -- -- 2 <5 10 4 <5 <10
110682 EL11570 110659-110689 13 43 19 281 125 1730 20 <5 990
110683 EL11570 110659-110689 23 21 -- 100 195 925 8 <5 660
110684 EL11570 110659-110689 <1 -- -- 4 35 25 10 <5 20
110685 EL11570 110659-110689 <1 -- -- 1 <5 15 2 <5 <10
110686 EL11570 110659-110689 <1 -- -- 2 15 10 4 <5 <10
110687 EL11570 110659-110689 <1 -- -- <1 35 15 2 <5 <10
110688 EL11570 110659-110689 <1 -- -- 47 105 395 4 <5 130
110689 EL11570 110659-110689 <1 -- -- 55 125 390 10 <5 80
