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GEOLOGICAL REPORT ON THE PERRIER BIG MAC
MASCOT JULIUS CAESAR AND SILVER HAWK CLAIMS
I1LJ r1J1N T S 82F 6W
490N 1170E
by Roy V Beavon B Sc Ph D
for
C ABER RESOURCES LTD
Vancouver B C 1st August 1982
MINERAL RESOL RCEs E RANCH
ASSESsttNT REPORT
TABLE o F CONTENTS
I INTRODUCTION
II PROPERTY
III HISTORY
IV GEOLOGY
1 Stratigraphyi Metasedimentary Rocks
ii Metavolcanic Rocks
iii Intrusive Rocks
2 Structure
i Foliation
ii Folding and Lineation
iii Faulting
3 Mineralization
V
VI
VII
VIII
IX
CONCLUSIONS AND RECOMMENDATIONS
BUDGET ESTIMATE
STATEMENT OF QUALIFICATIONS
COST STATEMENT
ILLUSTRATIONS
Map 1 Location of Property
Map 2 Claim Map
Map 3 Geological Map 1 540
Map 4 Plan and Section Perrier Mine 1932
PAGE NO
1
1
2
4
4
5
5
7
9
9
10
10
11
14
15
16
17
oI INTRODUCTION
The work described in this report was executed 5
to 7 km south of the city of Nelson B C in the drainagesof Cottonwood and Selous Creeks Cottonwood Creek runs
northward alongside the paved Highway No 6 and parallelto the Burlington Northern Railway Map 1 Access is
therefore on foot and by 2 wheel drive vehicle The mineral
showings may be reached by 4 wheel drive vehicles along old
logging roads that are currently in need of maintenance so
that access for this work was on foot Elevations of the
mapped area range from 3100 to 5300 ft
II PROPERTY
The property consists of thirteen claims which
include three reverted Crown Grants eight two post claims
one fraction and one reduced modified grid claim consistingof twelve units Map 2 Table 1 The writer checked legaland initial post locations for the Silver Hawk Big Mac and
Perrier Claims on the ground and these are shown on the
geological map Map 3 The precise location of the reverted
Crown Grants Julius Caesar and Mascot is doubtful and would
require tracing back to the original surveys
The thirteen claims shown in Table 1 are legallyand beneficially owned by Mr C pitman and Associates of
Nelson B C
Q
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4
YUKON NWTB
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AUFt Nelson
Prince Georve
Ft St ohn
II
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SELOUS CREEKPROPERTY 1
0
USA
ABER RESOURCES LTD
BEAVON CONSUlJING LTD
SELOUS CREEK PROPERTYNELSON M D B C
LOCATION MAP
200 BRITISH COLUMBIA400
100 200M LES SCALE I 120mil s FEB 1982 FIG I
CTABLE 1
CLAIM SCHEDULE
CLAIM LOCA TlON NO EXPIRY DA TE
Lizzie C 1852 July 3 1983
Mascot 1807 June 30 1983
Julius Caesar 1808 June 30 1983
Silver Hawk 1899 September 12 1982
Perrier 1 2033 December 1 1982
Perrier 2 2034 December 1 1982
Perrier 3 2035 December 1 1982
Perrier 4 2036 December 1 1982
Big Mac 1 2296 June 1 1983
Big Mac 2 2297 June 1 1983
Big Mac 3 2298 June 1 1983
Big Mac 4 2299 June 1 1983
Big Mac Fraction 2300 June 1 1983
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III HISTORY
There are few records of the early history of the
claim area The Perrier gold prospect was staked in 1910
and produced 2 804 tons of between 1 01 and 0 62 oz ton Au
in the early nineteen thirties Cockfield 1936 An under
ground plan by O Grady 1932 is enclosed Map 4 No records
of the other three reverted Crown Grants could be found
In 1960 Sheep Creek Gold Mines held an option on
the Big Mac claims and drilled five diamond drill holes for
a total footage of 791 feet beneath two lead zinc silver
showings shown as the North and South Showings on Map 2
Three holes were drilled on the South Showing and two holes
were drilled under the North Showing All the holes were drilled
eastwards but their precise location is not known Mr J
McIntosh of Delta C kindly supplied information from drill
logs in his possession that had low assay values in lead zinc
and silver See also B C M M Rept 1960
In 1970 the Big Mac claims were restaked as Silver
and Sam claims owned by Cop Mac Mines Ltd Geophysicalwork was done on the North and South showings including
electromagnetic VLF and JEM surveys which were found to be
ineffective in discrimination of mineralized ground In
addition a property wide geochemical survey was done at 400
ft line spacings and samples taken every 100 ft Copperlead and zinc were determined and several anomalies were
found and trenched without encouragement Assessment Report
3091
3
oA geological report was submitted to Warrior
Resources Ltd in 1978 on the John Claims restaked on the
Silver and Sam claims There are references to trenchingin 1971 and the North and South showings are documented
with assay plans by Tough and Taylor The geology was
outlined briefly and a detailed geological survey was
recommended B C Assessment Report 7377 Subsequentlyin 1979 the southern portion of the property was surveyedgeochemically for lead zinc and gold Anomalous goldvalues were found over gravel deposits west of the Perrier
prospect Assessment Report 3091
o
The purpose of present report is to document de
tailed mapping as recommended in Assessment Report 7377
and this was done in order to study the geological controls
of the base metal mineralization to study the gold occurrences
and to make recommendations for future work if warranted
Unfortunately the underground workings are in poor condition
and would require extensive work before they could be safelyentered
o
An area of 5 sq km within and adjoining the
claims was mapped geologically at a scale of 1 6720 using1980 air photographs courtesy of Crestbrook Logging Co of
Cranbrook B C These photographs which were blown up from
1 12000 to 1 6000 enabled precise definition of outcrop and
talus derived from outcrop together with old roads and old
trenches Traverses between known points were scaled usingtopo chain compass traverses A total of six working dayswere spent on the ground which contains at least six old
prospects All of the claims were covered with the exceptionof the less accessible parts of the Silver Hawk Claim where
line cutting will be necessary
o
o
4
IV GEOLOGY
The general geology of the Nelson and Yrnir areas
is well known from reports by Leroy 1912 Drysdale 1917
Cockfield 1936 McAllister 1951 and Little 1960
Mesozoic sedimentary and volcanic rocks of the Ymir and
Rossland Formations are deformed and intruded by the Nelson
granites The property under discussion is located to the
west of the main body of granitic rocks and is surrounded
by satellitic intrusions All the supracrustal rocks have
been affected by lower amphibolite grade of regional meta
morphism with the imposition of a variably developed folia
tion The results of the mapping are included in Map 3
1 Stratigraphy
The stratigraphy of ancient volcanic areas is often
difficult to establish due to the lack of abundant faunas to
the presence of faulting alteration and metamorphism and
to volcanic facies that do not behave in a layer cake
fashion The Nelson area is no exception but the writer
has attempted to break down the succession as far as is
practicable
By far the greater area of the claims is underlain
by metavolcanic rocks of the Rossland Formation but the
western and north western parts of the property contain meta
sedimentary rocks classified by Little 1960 as Unit B of
indeterminate age
o
o
o
5
i Metasedimentary Rocks
The metasedimentary rocks consist of we bedded
argi lites and si ty grits that contain poorly developedgraded bedding The fine grained shaly interbeds contain
abundant 15 disseminated pyrite Although graded beddingsuggests that these metasediments are older than the Rossland
Formation it is more likely that they are contemporaneouswith the volcanism since intercalations of similar rustysediments occur within the Rossland Formation near its
northwestern contact with the metasedimentary rocks
Near their northwestern contact with the Nelson
batholith the metasediments are transformed into schistose
grits and fine grained pelitic quartzites with increasingbiotite con tent
Southwest of Cottonwood Creek the metasediments
are clearly intercalated with schistose and massive green
stone lithologies Accordingly the Unit B of Little 1960
is here recognized as the Ymir Rossland transition rather
than a separate unit of indeterminate age
ii Metavolcanic Rocks
The bu k of the claims are underlain by andesitic
flow rocks cognate tuffaceous biotite schists and thin
intercalations of limestone and rusty argillite Proceedingfrom northwest to southeast across the claims the followingascending sequence of lithologies has been recognized Table 2
6
oTable 2 Subdivision of the basal Rossland Formation
d
c
b
a
Lithology
Biotite tuffites
Coarse porphyroblastic flows
Pillowed flows
Flow breccias pillow breccias
Approx thickness in m
240
550
30
425
Note that minor sedimentary and tuffaceous units are included
in all four subdivisions
a The flow breccias are typical hyaloclasticdeposits that are best observed on weathered surfaces Theyare usually moderately to well foliated greenstones containingflattened angular and ellipsoidal clasts in a similar green
matrix Phenocrysts are not common and since the foliation
is trans cted by hornblendic porphyroblasts these are
suspected to be of metamorphic origin Where present the
hornblende is often rounded as though replacing primaryamygdules
The flow breccias where poorly foliated contain
fragments 5 cm in diameter Minor differences in clast
composition can be attributed to subaqueous alteration rather
than accidental inclusions Pillow breccias contain flatten
ed ellipsoidal clasts up to 30 cm in length containing chill
ed margins reminiscent of pillow rims Note that the North
Showing occurs within the flow breccia horizon
o
b The true pillow lavas have an exposed thickness
of only 30 m They occur in massive jointed outcropsreminiscent of intrusive rocks pillow rims are well developedeven in unweathered situations but no top determinations
could be made The inter pillow areas are occupied by triang1alarareas of recrystallized chert
7
oc The pillowed zone is overlain to the south
east by 500 m of massive coarsely porphyritic porphyroblasticamphibolites that have been previously regarded as augiteporphyries Foliation is weakly developed and flow structures
are usually absent in this subdivision The coarsest
amphibolites reach gabbroic proportions immediately south
east of the South Showing
o
d The easternmost and uppermost member of the
volcanic succession consists of 250 m of medium to well
foliated biotitic tuffites These are often well banded with
sedimentary layering parallel to schistosity This member of
the Rossland Formation can be traced as far south as the
Perrier gold prospect where it hosts a narrow strattform
showing of base metals including magnetite Lucky Boyadit The subdivision of the volcanic rocks indicates that
three stratiform showings of base metals North South and
Lucky Boy occur at three different stratigraphic horizons
as defined by the volcanic facies of the Rossland Formation
iii Intrusive Rocks and Metamorphism
Major intrusive rocks of the Nelson Batholith
outcrop to the west and northwest of the property and fingerinto the claims on the west side of the Cottonwood ValleyThese intrusions consist of porphyritic biotite granite near
the western margin of the Silver Hawk Claim and equigranularbiotite granite on the Julius Caesar Claim
U
Only one normal contact was observed in a railwaycutting north of the northernmost railroad trestle This
contact appears concordant with quartzitic argillites but
when mapped northwards its behaviour is obliquely discordant
in relation to the wall rocks The south westernmost granite
8
ooccurrence is interpreted as a fault wedge but no contacts
are exposed So far as the writer is aware no granite was
recorded previously on the Mascot and Julius Caesar claims
Minor intrusive rocks were observed at several
localities notably feldspar porphyry basaltic feldsparporphyry and lamprophyre The feldspar porphyries are
common southeast of Cottonwood Creek where they occur as
northward striking transgressive sheets that dip to the east
at 50 degrees They vary in texture from a crowded feldsparporphyry 70 phenocrysts to virtually non porphyriticfelsite or rhyolite No flow structures were observed but
the marginal porphyries are often brecciated indicatingnear surface emplacement Locally these intrusions are
foliated but generally speaking they tend to be massive
o A narrow 1 m dike of crowded feldspar porphyryoccurs at the North Showing where it forms the footwall to
mineralized calcareous biotite tuffite horizon
Biotite lamprophyres occur in sill like narrow
intrusions at several localities As in the case of the
metavolcanic rocks the lamprophyres are massive to weaklyfoliated They are usually fine grained with 3 rom flecks of
biotite and an altered chloritized mafic phenocrysts set
in a dark green to black fine grained matrix In all cases
observed the contacts dip parallel to the bedding and folia
tion of the wall rocks The age of these ultramafic minor
intrusives is uncertain but they have not been observed
cutting any of the other intrusive rocks
o
9
oBasaltic porphyries were observed only in two
trenches one near the North Showing and one north of the
Lizzie e shaft Float samples near the former localitycontain xenoliths of feldspar porphyry A Tertiary age is
indicated by the fresh appearance and lack of foliation of
the basaltic porphyries
2 Structure
o
The most widely developed structure of the area
mapped is a steeply dipping foliation that varies in strike
from northeast in the northern two thirds of the claims to
southeast in the south Attendant folding is difficult to
recognize aside from small scale folds where foliation is
difficult to recognize The importance of faulting has not
been emphasized in previous reports but there is topo
graphic and quartz vein evidence of northwest to southeast
faults in several parts of the property
i Foliation
Foliation is developed with variable intensitythroughout the map area and wherever observed in conjunctionwith sedimentary bedding is usually a parallel structure
This implicates that isoclinal folds may be present but no
repitition of the volcanic horizons occuring across the strike
is evident from the mapping
Because foliation is absent in some members of the
andesitic volcanic rocks and well developed in others the
presence or absence of foliation in certain rock types is of
little value in age diagnoses
o
10
oThe variation in strike of the foliation from
northeast in the north to southeast in the south Map 3
is accompanied by a shallowing of the westward dip of
foliation in the intervening area notably west of Cottonwood
Creek This broad warping is clearly due to a mild late
folding of the foliation accompanied by a similar variation
in the plunge of b lineations
ii Folding
o
As stated above folding that accompanied to
formation of the foliation has not been recognized in the
claim area Minor folds which plunge south eastward have
been observed in argillites near the Lizzie C and in limyhorizons of both North and South showings Map 3 The plungeof the minor folds is similar to the southwestward plungeof the b lineations which are common in the foliated meta
volcanic horizons Together with the fact that most of the
granitic contacts are semi concordant with the supracrustalrocks this observation suggests that the intersection of the
granite with the mineralized horizons will be quite deep and
should not interfere with any drilling
iii Faulting
The structure of the claims is dominated by NW to SE
faulting that appears to control the direction of Cottonwood
Creek The evidence for this comes partly from an undergroundplan Map of the Perrier prospect by O Grady 1932 part y
from the distribution of rock types west of the valley Map 3
from physiographic evidence on air photos and from quartzvein occurrences throughout the claims
o
1
GIY E
Ii
IMLy SECTIOItcLInePEQJ2IEI2 MINE
T176 fJrlfis17 4m ccn Etf lorersJflitNELSON 0
00
lap
D kJ 2D
sCR FJiBT
l 5ECTOft A A
i iIl
I re lZoo0
11
Zoo tl
n
ItJf
Itf
rt ih
I
IOre
t300
3
IL
j
To Accompany 2eporf bl1klsid f Enqineer 8 OC7n
Ifteson 8C 1932f C 8uroau or MInes o
9I
t4l4i
mfO ST
I
OIET L
eo
5HAFT0
On
8D
t
400
A He
11
JThe physiographic evidence comes from sudden
changes in the hillside slopes to the north of Selous Creek
One of those faults may contain a surficial deposit of
travertine seen in float and coatings on outcrops At one
stage during mapping it was thought that the North showingand South showing were either separated by the NW faults or
repeated across the strike by folding but the mapping in
dicates that they are probably located at two different
horizons within the volcanic rocks and only indirectlyassociated with the northwest faults
o
Judging from O Grady s map of the Perrier Map 4
the NW striking faults dip steeply to the NE but they may
be vertical in other cases The throw of the NW fault at
the Perrier is down towards the SW so that this fault can
be classed as a high angle thrust fault In addition to
the Northwest trending faults a west north west strikingfault is shown on O Gray s map but none of these were
identifiable in the surface mapping A northeast strikingfault of unknown throw passes through the Lizzie C shaft
and is identified by fault gouge in one of the trenches
3 Mineralization
Three types of mineralization occur on the subjectclaims i quartz veins with gold potential ii dissemi
nated pyrite in meta tuffites and iii stratiform showingsof Pb Zn Ag Cu of possible contact metamorphic origin
u
i The close relationship between gold mineralizationat the Perrier prospect with northwest thrust faulting is
probably repeated at the Julius Caesar adit Both veins are
gently dipping at 27 to 30 degrees although the northeast
strike of the Perrier does not parallel the east to west
strike of the Julius Caesar It should be noted that magnetitecommonly accompanies pyrite in some of the mine dumps near
the Perrier
12
oThe Julius Caesar vein is hosted by quartz
feldspar porphyry that shows a tendency to quartz stockwork
developments Chip samples in and around the adit returned
only trace amounts of gold Table 3
ii About 550 m north of the Perrier a considerableamount of disseminated pyrite 15 30 occurs in bedrock andfloat composed of biotite tuffites of the Rossland volcanicformation Again chip samples failed to return any goldvalues Table 3
iii Three stratiform showings occur on the propertyOne of these is a narrow zone 45 cm wide about 150 m southof the Perrier shaft Known as the Lucky Boy adit the
assays shown in Table 3 were obtained
J TABLE 3
Assays and Rock Geochemistry Selous Creek Area
Assays
Locality
Lucky Boy dump grabLucky Boy portal across 45 cm
Lizzie c grab sample
Cu
165
190025
Pb
3 35
3 6640
Zn
10 75
5 75
3 49
Ag2 623 34
58
Au
031
079001
Rock Geochemistry
Locality
1 Dissem pyrite 550 m north of Perrier ProspectAu ppb
Sample No 0228 bedrock rock chip 5
Sample No 0229 bedrock rock chip 10Sample No 0230 float rock chip 5
Sample No 0231 float rock chip 5Sample No 0232 float rock chip 20
2 Julius Caesar aditAu ppb Ag ppm
Sample No 0233 bedrock chip 20 0 6Sample No 0234 bedrock chip 20 1 7
13
JThe values occur within schistose biotite tuffites
which exhibit weak to moderate sedimentary banding Minerali
zation consists of sphalerite galena magnetite and chalco
pyrite and appears to be crudely banded
The remaining stratiform occurrences were consideredto be skarn or shear zone desposits by previous workers
The North and South showings are described and sample results
are given in Assessment Report 7377 so this aspect of the
mineralization is not repeated here Suffice it to say that
erratic values of Zn Pb Ag Cu Au were returned over
mineable widths and short 100 to 150 ft strike lengths
The host rocks consist of a limey tuffaceous
biotite schist at the North showing and similar lithologiesgrade into limestone and marble host rocks at the South showingThe North showing contains well banded sphalerite indicative of
a volcanogenic or sedimentary deposition Sphalerite laminations
appear to thicken into the hinge zones of minor folds indicat
ing a pre foliation emplacement of mineralization
In addition to the sphalerite galena chalcopyriteand pyrite the writer identified magnetite at the North showingbut failed to find similar material at the South showing As
noted previously magnetite crudely banded was also found at
the Lucky Boy adit
o
The presence of an isolated 1 m dike of feldsparporphyry at the North showing is not repeated at any of the
other stratiform occurrences and is therefore not considered
a likely source for the mineralization It may be concluded
that a syn volcanic origin can be proposed for the base metal
showings of Selou Creek but that a replacement or skarn
origin cannot be ruled out of consideration From a practicalviewpoint it is surprising that no magnetic survey has been
undertaken on the Selons Creek property in spite of the use
of more sophisticated EM methods
14
v CONCLUSIONS RECOMMENDATIONS
The Selous Creek Property has received considerable
work in the past all without the recognition of magnetite in
two stratiform showings and the Perrier gold quartz area A
magnetometer survey could perform the dual service of outlin
ing interesting mineralization together with increasing geo
logical knowledge of this poorly exposed property
J
15
oVI BUDGET ESTIMATE
Stage 1
Line Cutting 20 000 m @ 150jkmMagnetometer Survey @ 150jkm
including base station rental
3 000 00
4 000 00
Total 7 000 00
Stage 2 contingent on results of Stage 1
Diamond Drilling 600 m @ 130jm 78 000 00
Signed R ovJLR V Beavon
Consulting Geologist
o
16
oVII STATEMENT OF QUALIFICATIONS
I Roy V Beavon of the City of Richmond in
the Province of British Columbia DO HEREBY CERTIFY
That I am a Consulting Geologist and a principalin Beavon Consulting Limited with offices located at
8720 Millmore Road Richmond British Columbia
I FURTHER CERTIFY THAT
l
U K
I am a graduate of the University College of Wales
with degrees of B Sc 1957 and Ph D 1960
2 I have been practising my profession continuouslyfor the past twenty two years
3 I am a Fellow of the Geological Association of
Canada of the Geological Society of London and of the
Geological Society of America and a Member of the Societyof Economic Geologists and the Canadian Institute of Miningand Metallurgy
4 The information for this report was obtained from
personal examinations of the properties on June 8 to June 131982 and from private reports and government publications
5 I have no direct interest in the property examined
this propertynor do I expect to receive any interest in
DATED at Richmond British Columbia this first dayof August 1982
8 MRoy V Beavon
Consulting Geologist
17
JVIII COST STATEMENT
Geological Mapping June 8 June 13
@ 250 per day 1 500 00
Transportation June 7 Richmond to
Nelson June 18 to Richmond800 miles @ 12 1 48 00
Board Lodging Meals7 days @ 40 280 00
Report Preparation 350 00
Assays and Rock Geochemistry Min En Labs Ltd 195 50
Air Photographs Pacific Survey Corp 103 98
Total 2 477 48
Note Receipts for 1st four items may be obtained from
Beavon Consulting Limited 8720 Millmore Rd
Richmond B C V7CIS9
Signed W6 J
J
REFERENCES
LEROY L E 1912 G S C Map 62A
DRYSDALE C W 1917 Ymir Mining Camp British ColumbiaG S C Memoir 94
O GRADY B T 1932 Plan and Section of the Perrier MineTo accompany B C Bureau of Mines Report by Resident
Engineer Nelson B C 1932
COCKFIELD W E 1936 Lode Gold Deposits of Ymir Ne1sonArea British Columbia G S C Memoir 191
MCALLISTER A L 1951 Yrnir Map Area British ColumbiaG S C Paper 51 4
LITTLE H W 1960 Nelson Map Area West Half BritishColumbia G S C Memoir 308
B C ASSESSMENT REPORTS 7377 7393
B C MINISTER OF MINES REPORTS 1910 1931 1960
JB C DEPARTMENT OF MINES BULLETIN 1932 pp 96 97
J
MIN EN Laboratories Ltd705 WEST 15th STREET
NORTH VANCOUVER B C CANADA V7M 1T2
TELEPHONE 604 9BO 5814
ANALYTICAL REPORT
Project Ne1son E aton a Date af reportJune 25 82
File No Z 22 Date somples recejved Jlgl e l 2 8 2
Samples submitted by
Report on
Aber Re s o urce
10rocks Geochem samples
Company
y4 Assay samples
Copies sent to
1 Abel Resources V ancouver B C
2
3
Somples Sieved to mesh Ground to mesh 80 rock ge oche m
100 assayPrepared samples stored Xl discorded 0
rejects ass aystored discarded iii geochem
Methods of analysis Assays Cu Pb Zn Ag Ac id d iges tion ch emica 1 ana lys i
Au Fire 1 s say G eQchem C u PbZn Agnitric p erch1oric d ig e s ti n
A A Au Aqua Regia A ARemarks
SPECIALISTS IN MINERAL ENVIRONMENTS
yTO Ab er
MIN EN LABORATORIES LTD i
705 WEST 15TH STREET NORTH VANCOUVER B C V7M 1T2 fPHONE 604 9905BI4 OR 604 9BB4 24
or t1
Qktrtificatf nfissag i cO c
Ran IrI
Res oUrc e sr PROJ ECTNoNe s OU lJ
ti01J5
DATE t
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oD ki Cn 0 An Q nn 1
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MINEEN Labora it jWAf
J
02
222
DATE
25
198275
801
70
65
60
55
SHEET T2
V7M 50
LYSISDATA
MIHENlaboratoriesLtd
5th51
NORTHVANCOUVERB
C
PHONE604980
5811
ffi
45II
9
Fe
ppm
ppm
GEOCHEMICA
0A
WEST35
70S30
u
ppb
Mn ppm
s ppm
Hg ppb
Co ppm
N ppm
16
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