2015 lucky thorne gold terrace British Columbia MLS Mining tech

Lucky 1025543 Claim Group John Bakus Event 5535009
____________________________________________________________________________________
____________________________________________________________________________________
February 7, 2015 Sookochoff Consultants Inc. page 1 of 24
JOHN BAKUS
(Owner & Operator)
GEOLOGICAL ASSESSMENT REPORT
(Event 5535009)
on a
STRUCTURAL ANALYSIS
Work done on
Tenures 1025543, 1025552, 1025553, 1032049, & 1032289
of the seven Tenure
Lucky 1025543 Claim Group
Skeena Mining Division
BCGS Map 103I.048
Centre of Work
6,037,646N, 536,752E (NAD 83)
Author & Consultant
Laurence Sookochoff, PEng
Sookochoff Consultants Inc.

____________________________________________________________________________________
____________________________________________________________________________________
TABLE OF CONTENTS
page
Summary ---------------------------------------------------------------------------- 4.
Introduction ------------------------------------------------------------------------ 5.
Property Description and Location ------------------------------------------- 5.
Accessibility, Climate, Local Resources, Infrastructure
and Physiography -------------------------------------------------------------- 6.
Water & Power -------------------------------------------------------------------- 6.
History: Property Area ----------------------------------------------------------- 7.
103I 095 GOLDEN NIB -------------------------------------------------- 8.
History: Property ------------------------------------------------------------------ 8.
103I 099 – LUCKY SEVEN ----------------------------------------------- 8.
Geology: Regional ----------------------------------------------------------------- 8.
Geology: Property Area --------------------------------------------------------- 8.
103I 095 - GOLDEN NIB ------------------------------------------------- 8.
103I 102 - EUREKA ------------------------------------------------------- 9.
103I 178 - BRUNSING ---------------------------------------------------- 9.
103I 095 - GOLDEN NIB -------------------------------------------------- 9.
Geology: Property ---------------------------------------------------------------- 9.
103I 091 – LA LIBERTAD ------------------------------------------------- 9.
103I 097 – PTARMIGAN ------------------------------------------------- 9.
103I 098 – PAUL ---------------------------------------------------------- 10.
103I 099 – LUCKY SEVEN ----------------------------------------------- 11.
103I 184 – SOCIETY GIRL ------------------------------------------------ 11.
Mineralization: Property Area ------------------------------------------------- 12.
103I 095 - GOLDEN NIB ------------------------------------------------- 12.
103I 102 - EUREKA ------------------------------------------------------- 12.
103I 178 - BRUNSING ---------------------------------------------------- 12.
Mineralization: Property -------------------------------------------------------- 12.
103I 091 – LA LIBERTAD ------------------------------------------------- 12.
103I 097 – PTARMIGAN ------------------------------------------------- 12.
103I 098 – ST.PAUL ------------------------------------------------------ 13.
103I 099 – LUCKY SEVEN ----------------------------------------------- 13.
103I 184 – SOCIETY GIRL ------------------------------------------------ 13.
Structural Analysis ---------------------------------------------------------------- 16.
Interpretation and Conclusions ----------------------------------------------- 20.
Selected References -------------------------------------------------------------- 22.
Statement of Costs --------------------------------------------------------------- 23.
Certificate --------------------------------------------------------------------------- 24.

____________________________________________________________________________________
____________________________________________________________________________________
Table of Contents (cont’d)
ILLUSTRATIONS
Figure 1. Location Map ---------------------------------------------------------- 5.
Figure 2. Claim Location --------------------------------------------------------- 7.
Figure 3. Claim Map -------------------------------------------------------------- 7.
Figure 4 Property Geology, Claim, Minfile, & Index Map --------------- 10.
Figure 5 Lucky Seven Molybdenum Anomaly ----------------------------- 15.
Figure 6 Society Girl Workings ------------------------------------------------ 17
Figure 7. Indicated Structures on five Tenures
of the Lucky Claim Group ------------------------------------------- 17.
Figure 8. Rose Diagram from Lineaments of
Tenures 547959 & 1014703 --------------------------------------- 17.
Figure 9. Cross-Structure & Minfile Locations on Google Earth ------- 18.
Figure 10. Conceptual model showing potential for deep-seated
Gold bonanza zones and/or porphyry Cu-Au ---------------- 19.
TABLES
Table 1. Mineral Tenures of the Kelly 547959 Claim Group ------------ 6.
Table 2. Minfile Structure Summary ----------------------------------------- 11.
Table 3. Minfile Mineralization Summary ----------------------------------- 16.
Table 4. Approximate UTM locations of cross-structures and Minfiles 19.
Table 4. Mineral Tenures of the Kelly 547959 Claim Group ------------ 6.

____________________________________________________________________________________
____________________________________________________________________________________
SUMMARY
The seven claim, 2009 hectare Lucky 1025543 Claim Group (“Property”) is located 682 kilometres
north of Vancouver, 123 kilometres east of Prince Rupert, a port city on the Pacific Ocean, and 11
kilometres south-southeast of Terrace. Air Canada provides daily service from Vancouver to Terrace
and the Canadian National Railway (CNR) provides services from Vancouver to Terrace and Prince
Rupert
The geology of the Property with the predominant Late Cretaceous granodioritic intrusives in a fault
contact with Tertiary granodioritic intrusives hosting polymetallic gold-silver and gold-silver bearing
quartz veins some of which exhibit epithermal qualities, indicates an encouraging geological condition
for the existence of a concealed mineralized copper-gold molybdenum porphyry resource.
There are many reported geological indicators, as noted in the Interpretations and Conclusions of this
report, on which to base this assumption, however, the foremost is at the Lucky Seven Minfile location
where soil analysis shows most of the highest gold values concentrated peripheral to the molybdenum
anomaly; which should be explored in detail for indications of a localized mineralized intrusive.
The structural analysis resulted in the delineation of three cross-structures from the intersection of
three indicated major structures; northerly, northwesterly, and easterly trending. Of the five Minfile
locations on the Property only the Society Girl Minfile correlated with a major structure and is located
between two cross-structures. As the Society Girl mineralized zone as well as other mineralized zones
may be episodic with variations in mineral content from polymetallic to silver and/or gold at telescopic
levels of deposition above an intrusive, the cross-structural locations should reveal the deep-seated
source of mineralization.
The Lucky Seven mineral zone, although not depicted on a major structure or a cross-structure, may be
associated with a localized area of structurally created weakness to allow the possible indication of
deep-seated porphyry molybdenum bearing material to show at surface.
Some of the reasons for initially exploring cross-structural areas are stated in the Interpretation and
Conclusions section and would include geological mapping of fracture density, alteration and alteration
products, and analysis for pathfinder and trace minerals which can offer a greater degree of
information than the analysis of a greater degree of primary minerals.
.

____________________________________________________________________________________
____________________________________________________________________________________
INTRODUCTION
In December 2014 a structural analysis was completed on five Tenures of the 903729 of the seven
claim Lucky 1025543 Claim Group (“Property”). The purpose of the program was to delineate cross-
structures which may be integral in geological controls to potentially economic mineral zones that may
occur on the Lucky 1025543 Claim Group
Information for this report was obtained from sources as cited under Selected References and from
the structural analysis as described herein.
Figure 1. Location Map
PROPERTY LOCATION AND DESCRIPTION
Location
The Property is situated within BCGS Map 103I.048 of the Skeena Mining Division, 682 kilometres
north of Vancouver, 11 kilometres south-southeast of Terrace, and 123 kilometres east-of Prince
Rupert, a port city on the Pacific Ocean.
Description
The Property is comprised of seven contiguous mineral claims covering an area of 375.7497 hectares.
Particulars are as follows.

____________________________________________________________________________________
____________________________________________________________________________________
Property Location and Description (cont’d)
Table 1. Mineral Tenures of the Lucky 1025543 Claim Group
Tenure
Number
Type Claim Name
Good
Until
Area
(ha)
1025539 Mineral
GOLDEN NIB 29T@ 55
GT AU
20190720 18.7837
1025543 Mineral
LUCKY SEVEN 91T@
68 GT AU
20190720 37.5824
1025552 Mineral
LUCKY S2 91 T@ 68
GT AU
20170120 56.3683
1025553 Mineral
ST PAUL SOCIETY 15
GT AU
20190120 93.9407
1032049 Mineral
THORNE LUCKY 7
MOLY
20171105 37.5826
1032289 Mineral Thorne La Libertad 20190120 75.1407
1032290 Mineral Thorne La Libertad W 20150228 56.3513
ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE
AND PHYSIOGRAPHY
Access
Access to the Property from Terrace is eastward via a network of paved roads for 10 kilometres to a
junction with a logging road which at a distance of four kilometers intersects the southern boundary of
Tenure 1032290. This road traverses most of Tenure 1032290 and the northeastern corner of Tenure
1025539 the westernmost claim of the Lucky 1025543 Claim Group.
As this logging road is the only road to access the lower timbered portion of the Property. To explore
the upper alpine areas of the Property, helicopter access from Terrace would be required.
Climate
The weather and temperatures are typical of the central and northwestern regions of British Columbia.
Snowfall can be expected from early October and lasting until late May with moderate rainfall during
the summer season.
Local Resources and Infrastructure
All resources to sustain a preliminary exploration program would be available at Terrace.
Air Canada provides a daily service to Vancouver and the Canadian National Railway (CNR) provides
services from Vancouver to Terrace and Prince Rupert.
Physiography
The topography is of moderate to steep forested slopes at the lower elevations to rugged slopes
approaching the central plateau-like ridge. Elevations range from 228 metres at the southwest corner
of the westernmost claim to between 1,420 and 1,450 metres along the northerly trending barren,
plateau-like ridge. The tree-line elevation is generally at 1,300 metres with a 50 metre variance.
WATER & POWER
In addition to a large lake near the tree-line in the southwest, there are many small lakes along the
ridge zone for any water requirements during the summer season. A 500 kv power line is within two
kilometres west of the Property.

____________________________________________________________________________________
____________________________________________________________________________________
Figure 2. Claims Location
(base map from MapPlace & Google Earth)
Figure 3. Claim Map
(from MapPlace)
HISTORY: PROPERTY AREA
The history of the MINFILE reported past producers peripheral to the Lucky 1025543 Claim Group is
reported as follows. The distance is relative to the Lucky 1025543 Claim Group.

____________________________________________________________________________________
____________________________________________________________________________________
History: Property Area (cont’d)
GOLDEN NIB Past Producer (Polymetallic veins Ag-Pb-Zn+/-Au, Subvolcanic Cu-Ag-Au (As-Sb))
MINFILE 103I 095
Within 100 metres south
In 1926, about 27 tonnes of hand-sorted ore were shipped from the Golden Nib property. From this
ore 1,493 grams of gold, 1,275 grams of silver and 302 kilograms of copper were recovered. Two
tonnes of ore were shipped to the Provincial Government sampling plant in Prince Rupert between
1938 and 1941. This shipment produced 124 grams of gold and 62 grams of silver.
HISTORY: PROPERTY
LUCKY SEVEN past producer (Polymetallic veins Ag-Pb-Zn+/-Au)
MINFILE 103I 099
Within Tenure 1035543
In 1918, about 91 tonnes of ore from the Lucky Seven claim group produced 6,221 grams of gold.
GEOLOGY: REGIONAL
Campbell (1967) describes the regional geology as:
Terrace, B.C. is located in a broad intermontane basin formed by the crossing of the present Skeena
Valley and what was probably a major preglacial river valley now partially occupied by the Kitimat
River. West and south of Terrace the Coast Range Mountains rise to 6500 feet, and east of Terrace the
Bulkley Ranges rise to 8000 feet. The elevation of the Terrace Basin is about 500 feet. The Zymoetz
River flows westward from the Bulkley Ranges to join the Skeena River at the northeast corner of the
basin. The Zymoetz Property is located in the Bulkley Mountains on the south side of the Zymoetz
River 21 miles east of Terrace. The principal showings, comprised of copper mineralization in a
sequence of volcanic rocks, are scattered over a distance of about one mile along the north flank of the
mountain that forms the south wall of the Zymoetz valley just west of the Clore River.
The Terrace basin is located on the eastern edge of the Coast Range batholith of granodioritic intrusive
rocks. The region west and south of Terrace is underlain predominantly by granodiorite intrusive rocks.
The area north and east of Terrace is underlain by Mesozoic formations that have been extensively
intruded by apophyses of granodiorite related to the batholith to the west.
The western fringe of the intruded rocks, within 16 miles east of Terrace, is comprised predominantly
of Triassic sedimentary rocks including limestones, sandstones and cherts. East of these rocks the
underlying formations are volcanic and sedimentary rocks of the Hazelton Group of Jurassic age.
GEOLOGY: PROPERTY AREA
The geology of the MINFILE reported showings and past producer peripheral to the Lucky 1025543
Claim Group are reported (Minfile records) as follows. The distance is relative to the Lucky 1025543
Claim Group.
GOLDEN NIB Past Producer (Polymetallic veins Ag-Pb-Zn+/-Au, Subvolcanic Cu-Ag-Au (As-Sb))
MINFILE 103I 095
A 1.5 to 4.5 metre wide shear zone, striking 045 degrees and dipping 70 degrees southeast, occurs
in coarse grained granodiorite of the Cretaceous to Tertiary Coast Plutonic Complex.

____________________________________________________________________________________
____________________________________________________________________________________
Geology: Property Area (cont’d)
Golden Nib (cont’d)
The zone, which is up to 300 metres long and 180 metres vertical distance, contains quartz lenses
and veins mineralized with pyrite and chalcopyrite. Associated alteration minerals include epidote,
chlorite and biotite. In the area of the main vein, remnants of older Mesozoic and Paleozoic
sedimentary rocks, mainly greywacke, have been altered to greenstone. North trending faults,
dipping 50 to 70 degrees west, cut the vein.
EUREKA showing (Porphyry Mo (Low F- type))
MINFILE 103I 102
One kilometre south-southeast
Molybdenite is associated with small, irregular, pegmatite dykes which intrude fine-grained granite
of the Cretaceous-Tertiary Coast Plutonic Complex.
BRUNSING showing (Intrusion-related Au pyrrhotite veins, L01: Subvolcanic Cu-Ag-Au (As-Sb)
MINFILE 103I 178
Four kilometres north
A shear zone in diorite of the Cretaceous to Tertiary Coast Plutonic Complex contains numerous
quartz stringers sparsely mineralized with pyrite, pyrrhotite and chalcopyrite
GEOLOGY: PROPERTY
The Property is indicated by the MapPlace geological download as covering two intrusives in a
northerly trending contact. To the west and predominant on the Property is a Late Cretaceous
granodioritic intrusive (LKgd). To the east the Property covers a small portion of a Tertiary granodioritic
intrusive (Tgd).
The geology on the MINFILE reported showings and past producers on the Lucky 1025543 Claim Group
are reported as follows (from Minfile records). The distance is relative to the Lucky 1025543 Claim
Group.
LA LIBERTAD showing (Polymetallic veins Ag-Pb-Zn+/-Au, Intrusion-related Au pyrrhotite veins)
MINFILE 103I 096
Granodiorite of the Cretaceous to Tertiary Coast Plutonic Complex is cut by quartz-feldspar porphyry
and later quartz diorite and lamprophyre. The lamprophyre dykes are cut by two parallel faults,
160 metres apart, striking 056 degrees and dipping 60 to 70 degrees southeast. Quartz veins, 0.2 to
1.0 metres wide, follow the faults and are mineralized with small seams of chalcopyrite, pyrite,
galena, tetrahedrite and sphalerite.
PTARMIGAN showing (Polymetallic veins Ag-Pb-Zn+/-Au)
MINFILE 103I 097
Granodiorite of the Cretaceous to Tertiary Coast Plutonic Complex contain small roof pendants of
sheared Mesozoic and Paleozoic greenstone derived from greywackes, volcanics and quartzites. The
roof pendants are 6 to 25 metres wide and contain quartz and carbonate veins parallel to the
northeast trending schistosity. The veins are sparsely mineralized with tetrahedrite, chalcopyrite,
pyrite, galena and sphalerite.

____________________________________________________________________________________
____________________________________________________________________________________
Geology: Property (cont’d)
Figure 4. Property Geology, Claim, Minfile, & Index Map
(Base map from MapPlace
GEOLOGY MAP LEGEND
Tertiary
Tgd
unnamed
granodioritic intrusive rocks
Late Cretaceous to Paleocene
LKPeqd
quartz dioritic intrusive rocks
Late Cretaceous
LKgd
unnamed
granodioritic intrusive rocks
Lower Jurassic
lJHT
Hazelton Group –Telkwa Formation
calc alkaline volcanic rocks
Devonian to Permean
DPSvc
Stikine Assemblage
volcanoclastic rocks
Devonian to Permean
DPSlm
Stikine Assemblage
Limestone, marble, calcareous
sedimentary rocks
ST. PAUL showing (Polymetallic veins Ag-Pb-Zn+/-Au, W Veins)
MINFILE 103I 098

__________________________________________________________________________________
__________________________________________________________________________________
February 7, 2015 Sookochoff Consultants Inc. Page 11 of 24
St. Paul (cont’d)
A 4.5 to 6.0 metre wide, east trending felsite dyke cuts massive biotite granodiorite and
lamprophyre dykes of the Cretaceous to Tertiary Coast Plutonic Complex.
Quartz veins, 0.2 to 1.4 metres wide, occur for several hundred metres along either side of the
dyke.
The St. Paul vein dips 40 degrees north and is mineralized with pyrite, chalcopyrite, galena,
sphalerite, arsenopyrite and gold. The vein occurs on the footwall side of the dyke, over a
distance of 670 metres.
MINFILE 103I 099
Granodiorites of the Cretaceous to Tertiary Coast Plutonic Complex are cut by numerous quartz
diorite and quartz-feldspar porphyry dykes. Quartz veins up to 2 metres in width, occur along a
600 metre, northeast trend. They are concentrated mainly along faults and along felsic dyke
margins. The wallrock is often schistose and contains sericite within about 25 centimetres of the
vein margins.
The quartz veins are comprised of off-white to pale grey, glassy to locally granular quartz.
Terminated, subhedral quartz crystals often line occasional vugs within the veins. Limonitic iron
oxides often coat fracture surfaces within the veins.
SOCIETY GIRL showing (Polymetallic veins Ag-Pb-Zn+/-Au)
MINFILE 103I 184
A 4.5 to 6.0 metre wide, east trending, felsite dyke cuts massive biotite granodiorite and
lamprophyre dykes of the Cretaceous to Tertiary Coast Plutonic Complex. Quartz veins, 0.2 to 1.4
metres wide, occur for several hundred metres along either side of the dyke.
The Society Girl vein, a continuation to the west of the St. Paul vein (103I 098), occurs on the
hangingwall side of the dyke. The vein is sparsely mineralized with pyrite, chalcopyrite, and
galena.
Table 2 Minfile structure summary
MINFILE Host Structure Strike Dip Comments
La Libertad Faults 056 65S Quartz vein
Ptarmigan Shear NE Polymetallic veins
St. Paul Shear 070 40N Quartz vein
Lucky Seven Faults NE Quartz veins
Society Girl E Quartz veins
beside dyke
MINERALIZATION: PROPERTY AREA
The mineralization on MINFILE reported showings and past producers peripheral to the Lucky
1025543 Claim Group are reported (Minfile records) as follows. The distance is relative to the Lucky
1025543 Claim Group.

__________________________________________________________________________________
__________________________________________________________________________________
GOLDEN NIB past producer (Polymetallic veins Ag-Pb-Zn+/-Au, Subvolcanic Cu-Ag-Au (As-Sb))
MINFILE 103I 095
Mineralization is erratic with lenses up to 2 metres and assays up to 7.7 grams per tonne gold and
14 grams per tonne silver (Assessment Report 11335). A grab sample assayed 4.2 grams per
tonne gold, 26.1 grams per tonne silver and 1.20 per cent copper (Assessment Report 13104).
EUREKA showing (Porphyry Mo (Low F- type))
MINFILE 103I 102
One kilometre south-southeast
Molybdenite is associated with small, irregular, pegmatite dykes which intrude fine-grained
granite of the Cretaceous-Tertiary Coast Plutonic Complex. The mineralization, which occurs
disseminated and in patches over a 30 by 60 metre area, consists of pyrite and molybdenite with
associated muscovite, tourmaline and epidote. A selected sample assayed 11.2 per cent
molybdenum and trace gold and silver (Minister of Mines Annual Report 1929).
BRUNSING showing (Intrusion-related Au pyrrhotite veins, L01: Subvolcanic Cu-Ag-Au (As-Sb)
MINFILE 103I 178
Four kilometres north
A shear zone in diorite of the Cretaceous to Tertiary Coast Plutonic Complex contains numerous
quartz stringers sparsely mineralized with pyrite, pyrrhotite and chalcopyrite. The veins carry
gold.
MINERALIZATION: PROPERTY
The mineralization on MINFILE reported showings and past producers on the Lucky 1025543 Claim
Group are reported as follows (from Minfile records).
LA LIBERTAD showing (Polymetallic veins Ag-Pb-Zn+/-Au, Intrusion-related Au pyrrhotite veins)
MINFILE 103I 096
A grab sample assayed 66 grams per tonne gold and 17 grams per tonne silver (Minister of Mines
Annual Report 1930). A sample of a quartz vein in the area assayed 0.07 per cent zinc
(Assessment Report 13104).
PTARMIGAN showing (Polymetallic veins Ag-Pb-Zn+/-Au)
MINFILE 103I 097
A sample of a 2.4 metre wide mineralized zone assayed 150 grams per tonne silver (Minister of
Mines Annual Report 1918) and a 4.6 metre chip sample assayed 55 grams per tonne silver and
0.3 grams per tonne gold (Minister of Mines Annual Report 1930). A selected sample of
tetrahedrite and pyrite assayed 460 grams per tonne silver and trace gold (Geological Survey of
Canada Memoir 205).

__________________________________________________________________________________
__________________________________________________________________________________
Mineralization: Property (cont’d)
ST. PAUL showing (Polymetallic veins Ag-Pb-Zn+/-Au, W Veins)
MINFILE 103I 098
A 7 centimetre channel sample of a sulphide rich zone, up to 1 metre wide, assayed 15.8 grams
per tonne gold, 92.6 grams per tonne silver, 0.04 per cent copper, 1.88 per cent lead and 0.08 per
cent zinc. A 1.4 metre channel sample assayed 5.7 grams per tonne gold, 3.43 grams per tonne
silver, 0.006 per cent copper, 0.11 per cent lead and 0.09 per cent zinc (Assessment Report 13104).
A quartz vein, located about 250 metres to the southeast is also mineralized with scheelite and
barite. Scheelite nodules as large as 7.62 centimetres in diameter were reported from this vein on
the St. Paul claim.
MINFILE 103I 099
Sulphide minerals within the quartz veins are pyrite, chalcopyrite, galena, sphalerite, tetrahedrite
(freibergite) and stephanite with rare visible gold occurring in the Lucky Seven vein. Pyrite is the
most abundant sulphide and occurs as disseminations within the veins; the other sulphides usually
occur as irregular, discontinuous masses. The mineralization is often concentrated near the vein
margins. Chalcopyrite occurs as irregular masses up to 2 centimetres in diameter occasionally
with malachite and/or azurite. Galena is present in several of the veins and locally, has been
partly altered to cerussite (?). Several quartz veins contain siderite and minor calcite.
Sample TT-9, from a quartz vein with galena, pyrite and chalcopyrite near the old adits assayed
7.16 grams per tonne gold, 38.3 grams per tonne silver, 0.246 per cent lead, 0.03 per cent zinc
and 0.015 per cent copper. Another sample taken from the dump pile at an old open cut assayed
0.695 grams per tonne gold, 99.5 grams per tonne silver, 2.533 per cent lead, 0.035 per cent zinc
and 0.161 per cent copper (Di Spirito, 1986).
About 460 metres to the southwest of the old workings, a sample from a 4 metre wide quartz vein
assayed 6.7 grams per tonne gold, 1049 grams per tonne silver, 0.094 per cent lead, 0.032 per
cent zinc, 0.024 per cent copper and 0.0012 per cent molybdenite (Assessment Report 13140).
In 1918, about 91 tonnes of ore from the Lucky Seven claim group produced 6,221 grams of gold.
SOCIETY GIRL showing (Polymetallic veins Ag-Pb-Zn+/-Au)
MINFILE 103I 184
A 76 centimetre sample assayed 6.9 grams per tonne gold and 17.1 grams per tonne silver
(Minister of Mines, Annual Report 1914). A sample of a quartz vein, which is likely part of the
Society Girl vein, assayed 0.3 grams per tonne gold, 13.7 grams per tonne silver, 0.01 per cent
copper, 1.08 per cent lead, and 0.02 per cent zinc (Assessment Report 13104).
In 1986, sample TT-45 was collected from the quartz vein exposed in the adit on the Society Girl
claim and assayed 1.19 grams per tonne gold. The quartz vein contains massive pyrite and trace
to 2.0 per cent chalcopyrite and galena across a 70 centimetre width (Di Spirito, et al., 1986).

__________________________________________________________________________________
__________________________________________________________________________________
Figure 5. LUCKY SEVEN MOLYBDENUM ANOMALY
(Map from Ostler 2008)
Ostler (2008) provides a description of the Lucky Seven molybdenum as:
The writer found that molybdenum concentrations ranged up to 82 ppm in the 1986 soil samples.
Upon contouring those results at 5, 10, and 25 ppm, he found that they formed a significant
anomaly in the southeastern part of the 1986 grid (Figures 7, and 11 to 15). The anomaly was
located just up hill from the main Lucky seven workings and had most of the high soil gold
concentrations around its periphery.
The 1986 soil-molybdenum anomaly extended off the Shangri-La grid for some unknown distance
eastward onto ground currently covered by the RABERTA #4 (538702) claim. The current (2008)
Lucky Seven soil survey was conducted in an effort to define an eastern extension of the 1986
anomaly. The 2008 survey identified two lobes on the eastern margin of the Lucky Seven soil-
molybdenum anomaly and thus was considered to have been successful (Figure 11).

__________________________________________________________________________________
__________________________________________________________________________________
Mineralization: Property (cont’d)
Society Girl (cont’d)
The Sadie showing, located just north of the Society Girl, is comprised of a 1.0 metre wide quartz
vein containing chalcopyrite, pyrite, malachite and azurite. A 30 centimetre sample taken from
this vein in 1929, assayed trace gold, 55 grams per tonne silver and 9.0 per cent copper (Minister
of Mines Annual Report 1929, page 78).
Mineralogical studies of the Society Girl quartz vein shows that it also contains small amounts of
covellite and arsenopyrite. Sphalerite is locally abundant within this vein. Chalcopyrite occurs as
irregular masses up to 2 centimetres in diameter with associated malachite and azurite. Goethite
occurs as a minor alteration product of pyrite in the western portion of the Society Girl vein
(DiSpirito et al. 1986).
Figure 6. SOCIETY GIRL WORKINGS
(Map from Ostler 2008)

__________________________________________________________________________________
__________________________________________________________________________________
Table 3 Minfile mineralization summary
(Information from Minfile records)
Minfile Sampl
e Type
Yea
r
Gol
d
g/t
Silver
g/t
Comments/References
La
Libertad
Grab 198
9
66.
0
17.0 Northern Miner September 4,
1989
La
Libertad
Bulk 192
9
76.
2
6,856 grams of gold from 90
tonnes
Ptarmiga
n
Grab 193
7
Tr 460.
0
GSC Memoir 205, p 28
St. Paul Chann
el
198
4
15.
8
92.6 7 cm wide; AR 13,104
Lucky
Seven
Chip 198
6
7.6 38.3 Property File - DiSpirito, et al
Lucky
Seven
Mined 191
8
6,221 grams gold from 91
tonnes
Society
Girl
Rock 198
4
0.3 13.7 AR 13,114
STRUCTURAL ANALYSIS
The Structural Analysis of five Tenures of the Lucky 1025543 Claim Group was accomplished by
marking the observed lineaments on a DEM Image hillshade map downloaded from MapPlace. A total
of 63 lineaments were indicated as shown on Figure 5. A Georient 32v9 software program was used
to create a Rose Diagram reflecting the grouping of the lineaments into an individual 10 °class sector
angle interval as shown on Figure 6.

__________________________________________________________________________________
__________________________________________________________________________________
Structural Analysis (cont’d)
Figure 7. Indicated Structures on five Tenures of the Lucky 1025543 Claim Group
(Base map: MapPlace & Google)
Figure 8. Rose Diagram from the Lineaments of five Tenures of the Lucky
1025543Claim Group

__________________________________________________________________________________
__________________________________________________________________________________
STATISTICS (for Figure 5)
Axial (non-polar) data
No. of Data = 63
Sector angle = 8°
Scale: tick interval = 2% [1.3 data]
Maximum = 15.9% [10 data]
Mean Resultant dir'n = 132-312
[Approx. 95% Confidence interval = ±71.1°]
(valid only for unimodal data)
_________________________
Mean Resultant dir'n = 132.5 - 312.5
Circ.Median = 135.0 - 315.0
Circ.Mean Dev.about median = 38.1°
Circ. Variance = 0.36
Circular Std.Dev. = 54.59°
Circ. Dispersion = 14.67
Circ.Std Error = 0.4826
Circ.Skewness = 0.21
Circ.Kurtosis = -2.86
kappa = 0.33
(von Mises concentration param.
estimate)
Resultant length = 10.25
Mean Resultant length = 0.1627
'Mean' Moments: Cbar = -0.0142; Sbar = -
0.1621
'Full' trig. sums: SumCos = -0.8966; Sbar = -
10.2112
Mean resultant of doubled angles = 0.223
Mean direction of doubled angles = 169
(Usage references: Mardia & Jupp,
'Directional Statistics', 1999, Wiley;
Fisher, 'Statistical Analysis of Circular Data',
1993, Cambridge University Press)
Note: The 95% confidence calculation uses
Fisher's (1993) 'large-sample method'
Figure 9. Cross-structure & Minfile locations on Google Earth
(Base map from MapPlace & Google Earth)

__________________________________________________________________________________
__________________________________________________________________________________
Table 3. Approximate UTM locations of Figures 5 & 7 cross-structures and
Minfiles
(UTM-NAD 83 Zone 9)
Area UTM East UTM
North
Elevation
(metres)
A 537,383 6,037,563 1,286
B 536,571 6,038,266 1,456
C 536,563 6,037,343 1,231
La Libertad 536,056 6,038,648 1,415
Ptarmigan 536,779 6,038,190 1,430
St. Paul 537,146 6,037,266 1,370
Lucky Seven 535,890 6,036,792 800
Society Girl 536,875 6,037,418 1,335
Figure 10. Conceptual model showing potential for deep-seated gold bonanza zones
and/or porphyry Cu-Au.
(Map from Bisson, 2014)

__________________________________________________________________________________
__________________________________________________________________________________
INTERPRETATION and CONCLUSIONS
Three cross-structures that were delineated on the five claims of the Lucky 1025543 Claim Group
would be the most prospective areas to explore for surficial geological indicators of a potential
economic mineral resource. This supposition is based on three important qualifying aspects that a
cross-structural location may generate for the geological indications of, in the case of the Lucky
property, a concealed bulk tonnage porphyry copper-gold molybdenum deposit.
 the cross-structure would likely be depth intensive to source, and/or provide an avenue for
hydrothermal fluids to reach the surface;
 the cross-structural location would probably create an expansive zone of fracturing from a
central breccia or intensely fractured zone for the deposition of the hydrothermal fluids;
 the cross-structural location would certainly leave surficially etched “fingerprints” of the
hydrothermal fluid composition or alteration products for the explorationist to record and
interpret as to the probability for a porphyry related mineral resource.
The more apparent geological indicators to a mineral resource on the Property include:
 the many mineral showings of the polymetallic veins and mainly the gold bearing quartz
veins;
 the mineralization of molybdenum with trace gold and silver at the Eureka Minfile showing
(MINFILE 103I.102) hosted by a Tertiary granodioritic intrusive one kilometre from the
Property;
 the molybdenum in soil anomalous values in the Lucky Seven area;
 the gold values concentrated around the periphery of the molybdenum anomaly (exemplify
a mini porphyry);
 the epithermal qualities of some of the quartz veins;
 the mineralization in the shear zones as an indication of surface seepage.
The strength of one of the delineated structures is shown at the Society Girl (Minfile 103I.097) Minfile
location which correlates with and is located on the AC structure and between cross-structures A & C.
The Society Girl structure which hosts a felsite dyke and adjacent mineralized quartz veins, is
reported to occur over several hundred metres. The mineralized zone at the cross–structural
locations should be more extensive and should provide a greater degree of explorative geological
information on a mineral source. Information as to pathfinder and trace minerals in addition to types
of alteration and alteration products should provide evidences as to the depth and mineral
constituents of the mineral source.
Thus, the Lucky 1025543 Claim Group reveals many positive geological features to the presence of an
economic mineral resource. The results of the structural analysis provided three cross-structural
areas for primary exploration where the analysis of structural controls and the interpretation of
surficial geological indicators could lead to the discovery of a concealed mineral resource.

__________________________________________________________________________________
__________________________________________________________________________________
Respectfully submitted
Sookochoff Consultants Inc.
Laurence Sookochoff, PEng

__________________________________________________________________________________
__________________________________________________________________________________
SELECTED REFERENCES
Allen, D.G. – Geochemical Assessment Report on the Mount Thornhill Gold Prospect for Seastar
Resource Corporation. September 19, 1984. AR 13,104.
- Geochemical, Geological and Geophysical Assessment Report on the Mount Thornhill
Property for Seastar Resource Corporation. September 16, 1985. AR 14,560.
Daughtry, K.L. – Prospecting and Geochemical Assessment Report on the Winfield Creek Property
for D.A. Davidson and Partners. January 21, 1992. AR 22,077.
MacIntyre, D.G., Desjardins, P., et al – Jurassic Stratigraphic Relationships in the Babine and
Telkwa Ranges (93L/10), 11,14,15)
MapPlace – Downloads
Marshak, S., Mitra, G. – Basic Methods of Structural Geology. pp 258-259, 264*.Prentice-Hall
Inc. 1988.
MtOnline - MINFILE downloads.
103I 091 – LA LIBERTAD
103I 095 GOLDEN NIB
103I 097 – PTARMIGAN
103I 098 – ST.PAUL
103I 099 – LUCKY SEVEN
103I 102 - EUREKA
103I 178 - BRUNSING
103I 184 – SOCIETY GIRL
Ostler, J. - Prospecting, Geological, Soil Geochemical, 3-D Induced Polarization, and Ground
Magnetic Surveys on the Central Thorne Property for Thorne Explorations Ltd. November 18, 2008.
AR30,316.

__________________________________________________________________________________
__________________________________________________________________________________
STATEMENT OF COSTS D
Work on the five Tenures of the Lucky 1025543 Claim Group was performed from December 4,
2014 to December 8, 2014 to the value as follows:
Structural Analysis
Laurence Sookochoff, PEng. 3 days @ $ 1,000.00/day ------------ $ 3,000.00
Maps -------------------------------------------------------------------------- 1,000.00
Report ------------------------------------------------------------------------- 3,500.00
$ 7,500.00
========

__________________________________________________________________________________
__________________________________________________________________________________
CERTIFICATE
I, Laurence Sookochoff, of the City of Vancouver, in the Province of British Columbia, do hereby
certify:
That I am a Consulting Geologist and principal of Sookochoff Consultants Inc. with an address at Suite
120 125A-1030 Denman Street, Vancouver, BC V6G 2M6.
I, Laurence Sookochoff, further certify that:
1) I am a graduate of the University of British Columbia (1966) and hold a B.Sc. degree in Geology.
2) I have been practicing on profession for the past forty-eight years.
3) I am registered and in good standing with the Association of Professional Engineers and
Geoscientists of British Columbia.
4) The information for this report is based on information as itemized in the Selected Reference section
of this report.
5) I have no interest in the Property as described herein.
Laurence Sookochoff, P. Eng.

2015 lucky thorne gold terrace British Columbia MLS Mining tech

Recommended

Recommended

More Related Content

More from John Bakus MLS Mining

More from John Bakus MLS Mining (7)

Recently uploaded

Recently uploaded (20)

2015 lucky thorne gold terrace British Columbia MLS Mining tech