Vendome ni 43 101

TECHNICAL REPORT

ON THE POLYMETALLIC

RESOURCES ON THE

San Javier, La Diana, and Fiscal 2012 Properties

State of Guerrero,
Mexico
ON BEHALF OF

VENDOME RESOURCES
CORP.
133 Richmond Street West
Suite 403,
Toronto, Ontario,
Canada, M5H 2L3

Report for NI 43-101

BY:

G. S. CARTER, P. ENG.

October 17, 2012

BROAD OAK ASSOCIATES

365 Bay Street
Suite 304
Toronto, Ontario
Canada, M5H 2V1

Vendome Properties 1 Broad Oak Associates

Date and Signature Page

CERTIFICATE of AUTHOR

I, Geoffrey S. Carter P. Eng., do hereby certify that:

1 I am a Principal of:
Broad Oak Associates
365 Bay Street, Suite 304
Toronto, Ontario,
Canada, M5H 2V1

2. I graduated with an Honours Bachelor of Science (1968) degree in Mining Engineering
from University of Wales, University College Cardiff, South Wales, UK in 1968

3. I am a member of the Professional Engineering Association of Manitoba, (5341) and I am
a Professional Engineer in Ontario, (100084354). I am also a member of the Canadian
Institute of Mining and Metallurgy.

4. I have practiced my profession in excess of forty years.

5. I have read the definition of “qualified person” set out in National Instrument 43-101
(“NI 43-101”) and certify that by reason of my education and past relevant work
experience, I fulfill with requirements to be a “qualified person” for the purposes of NI
43-101. This report is based on my personal review of information provided by the
Issuer and on discussions with the Issuer’s representatives. My relevant experience for
the purpose of this report is:

 Anglo American Corporation 1968-1983, Mine Engineer, General Mine Foreman,
Hudson Bay Mining and Smelting Limited, Vice President Operations Inspiration
Coal.
 Senior Mining Engineer - Project Technical Evaluation Hudson Bay Mining and
Smelting Co. Limited 1980-1981
 Mining Analyst, Midland Doherty, 1983-1986
 Author of several Technical Reports, 2002-2012

6. I am responsible for the preparation of the technical report and titled Technical Report on
the Polymetallic Resources on the San Javier, La Diana, and San Miquel Properties, dated
October 17, 2012, (the Technical Report). I visited the property on July 6 and 7, 2010
and again on December 5 and 6, 2011.

7. I have had no prior involvement with the properties that are the subject of the Technical
Report.


8. As of the date of this certificate, to the best of my knowledge, information and belief, the
technical report contains all scientific and technical information that is required to be
disclosed to make the technical report not misleading.

9. I am independent of the issuer applying all of the tests in section 1.5 of National
Instrument 43-101.

10. I have read National Instrument 43-101 and Form 43-101F1, and the Technical Report
has been prepared in compliance with that instrument and form.

11. I consent to the filing of the Technical Report with any stock exchange and other
regulatory authority and any publication by them for regulatory purposes, including
electronic publication in the public company files on their websites accessible by the
public, of the Technical Report.

Dated the 17th day of October, 2012.

Seal or Stamp
Geoffrey S. Carter

Printed name of Geoffrey S. Carter, P. Eng.

Geoffrey S. Carter
Broad Oak Associates
365 Bay Street, Suite 304
Toronto, Ontario
Canada, M5H 2V1
Tel: 416-594-6672
Fax: 416-594-3446
Email: BOA@Broadoak.ca


TABLE OF CONTENTS
Page Number
1.0 Summary 6
2.0 Introduction 7
3.0 Reliance on Other Experts 7
4.0 Property Description and Location 8
5.0 Accessibility, Climate, Local Resources, Infrastructure, and Physiography 12
6.0 History 13
7.0 Geological Setting and Mineralization 16
8.0 Deposit Types 19
9.0 Exploration 19
10.0 Drilling 36
11.0 Sample Preparation, Analyses, and Security 36
12.0 Data Verification 39
13.0 Mineral Processing and Metallurgical Testing 41
14.0 Mineral Resource Estimates 41
15.0 Mineral Reserve Estimates 41
16.0 Mining Methods 42
17.0 Recovery Methods 42
18.0 Project Infrastructure 42
19.0 Market Studies and Contracts 42
20.0 Environmental Studies, Permitting and Social or Community Impact 42
21.0 Capital and Operating Costs 42
22.0 Economic Analysis 42
23.0 Adjacent Properties 43
24.0 Other Relevant Data and Information 45
25.0 Interpretation and Conclusions 45
26.0 Recommendations 49
27.0 References 52


Figure Page

Fig. 1 General Location of San Javier Project 9
Fig. 2 General Location in Guerrero State 10
Fig. 3 Topography Map Showing 3 Concessions 11
Fig. 4 San Javier typical topography Mixtecapa River 13
Fig. 5 Map Showing Location of San Javier and other mineral deposits 14
Fig. 6 Regional Geology 17
Fig. 7 Possible Felsic Crystal Tuff 18
Fig. 8 Maguey Granite 18
Fig. 9 Satellite Imagery Regional Interpretations 21
Fig.10 Satellite Imagery Interpreted Alteration Zones 22
Fig.11 Property Geology from Satellite Imagery 23
Fig.12 Silver in Soils 25
Fig.13 Arsenic in Soils 26
Fig.14 Copper in Soils 27
Fig.15 Lead in Soils 28
Fig.16 Zinc in Soils 29
Fig.17 Silver in Chip Samples 31
Fig.18 Arsenic in Chip Samples 32
Fig.19 Lead in Chip Samples 33
Fig.20 Stream Sediment Sample Sites 34
Fig.21 Sample Locations July 2010 39
Fig.22 Grab Sample Locations December 2011 40
Fig.23 San Javier, La Diana and Fiscal 2012 Properties 43
Fig.24 Satellite Imagery Interpretation Map 44
Fig.25 Vein Locations San Javier Property 47
Fig.26 Vein Locations North Portion San Javier Property 48
Fig.27 Vein Locations South Portion San Javier Property 48

Consent of Author 53


1.0 Summary

Vendome Resources Corp. (“Vendome” or “Company”) is a Toronto, Canada based public
mineral exploration company. On December 1, 2011 Vendome announced that its wholly-
owned Mexican subsidiary (Vendome Minas, S.A. de C.V.) had entered into an agreement to
acquire from Camsim Minas S.A. de C.V. (“Camsim”) an earn-in option for a 50% undivided
interest in and to the San Javier Mine property, located within the municipality of Malinaltepec,
State of Guerrero, Mexico. Vendome paid CDN $75,000 cash and issued 1,000,000 common
shares to Camsim upon signing of the earn-in option agreement. Vendome has also agreed to
issue 1,000,000 common shares to Camsim on each of the first and second anniversaries of the
effective date of the agreement, and make a final cash payment of CDN $250,000 to Camsim on
the third anniversary date.

Vendome entered into an agreement via its wholly-owned Mexican subsidiary (Vendome Minas,
S.A. de C.V.) to acquire from Camsim Minas S.A. de C.V. (“Camsim”) an earn-in option for a
50% undivided interest in and to the La Diana property, located within the municipality of
Malinaltepec, State of Guerrero, Mexico on September 2, 2010, which was amended on February
23, 2012. The amended date became the anniversary date for the following payments. Vendome
paid CDN $75,000 cash and issued 1,000,000 common shares to Camsim upon signing of the
earn-in option agreement. Vendome has also agreed to issue 1,800,000 common shares to
Camsim on the first anniversary and 1,000,000 shares on the second anniversary of the effective
date of the amended agreement, and make a final cash payment of CDN $250,000 to Camsim on
the third anniversary date. Vendome agreed to a work commitment of $2,600,000 over the three
year period.

The San Miquel property was acquired (100% of the mineral rights) from Santa Claws Minas, S.A.
DE C.V. for $25,000 and 2,500,000 Vendome shares on August 3, 2011.

The San Javier, La Diana,and San Miquel polymetallic projects are located 135 kilometres
southeast of the city of Hermosillo, State of Guerrero, in northwestern Mexico. The San Javier
project is contained in a single concession of 253 hectares. This is the only project on which
exploration apart from satellite imagery has been carried out.

ACA Howe International Limited (“ACA Howe”) has visited the property and was responsible
for running Vendome’s exploration program.

In the spring of 2012, Howe conducted and managed an early stage exploration program on the
San Javier property on behalf of Vendome. The detailed results of this program are given in
section 9 of this report. Two drill targets were identified during this program and will drilled
during phase 1. The present satellite imagery suggests the potential for similar targets on the
other properties. Vendome has nearly 17,000 hectares between the three properties.

Broad Oak recommends a two phase exploration program on this large property position, and the
details are given in section 26 of this report. Phase one is budgeted at US$3,210,800, and phase
two which is contingent on the results of phase one is budgeted at US$3,124,550. These
programs should be completed in the next 12-24 months.


2.0 Introduction

Broad Oak Associates (“Broad Oak”) was engaged by Vendome Resources Corp. to provide an
independent technical report. This report was prepared under the direction of Geoffrey S. Carter, P.
Eng., a principal of Broad Oak and a Qualified Person. A site visit was made to the property on
July 6 and 7, 2010 and again on December 5 and 6, 2011 when grab samples were taken. The
extensive database that Vendome has assembled in their offices in Toronto, Canada has been made
fully available to Broad Oak.

The exploration conducted on the properties was carried out by ACA Howe for Vendome in 2012.

3.0 Reliance on Other Experts

Broad Oak relied upon Vendome personnel and consultants and their corporate counsel for
information regarding the current status of legal title of the property, property agreements, corporate
structure, permits and any outstanding environmental orders.


4.0 Property Description and Location

The Projects are located approximately135 kilometres east-northeast from the city of Acapulco,
and approximately 4 kilometres east of the village of Barranca Panal, in the south east part of the
State of Guerrero, southern Mexico. The property is approximately 6 hours from Acapulco by
road via Marquela. Access to the San Javier property is possible by 4 wheel drive vehicle in
good weather, but difficult in the rainy season. Access to La Diana and San Miquel is very
limited as there are few roads.

As of April 28, 2005 the historical distinction between exploration and exploitation concessions
was replaced by the establishment of mining concessions, which confers upon its holders the
rights to exploration, exploitation and extraction of substances. The Project consists of three
Mining Concessions which covers 16,865 hectares.

The duration of the concessions is 50 years from the date of request with the potential to renew
for a further 50 years. Rental fees must be paid twice a year (end of January and end of July).
Effective from January 1, 2012 fees required during the first and second years in Mexican Pesos
are $8.05 per hectare; for the third and fourth years a payment of $7.60 per hectare; during the
fifth and sixth year payment of $15.72 per hectare; during the seventh and eighth years payment
of $31.62; in the ninth and tenth years payment of $63.22 per hectare and from the eleventh year
payment of $111.27. Payment for the San Javier project concession in the year 7 (2012) is
$7,999.86 Mexican Pesos. Further payments are required for the La Diana and San Miquel
concessions.

Table 1. San Javier, La Diana, and San Miquel Mining Concessions

Concession Certificate Owner Area Staking Date Expiration
Name Number (Hectares) Date
San Javier 181899 Cansim Minas, S.A. DE 253 July 6/2005 July 6/2055
C.V
La Diana 234454 Cansim Minas, S.A. DE 14,722 June 30/2009 June 29/2058
C.V
San Miquel 237866 Santa Claws Minas, S.A. 1,890 May 17/2011 May 16/2061
DE C.V.

Note documentation is being processed to transfer San Miquel into Vendome Minas, S.A. de C.V.,
the wholly owned Mexican subsidiary of Vendome.


Fig. 1, General Location of San Javier Project


Fig. 2, General Location of San Javier Project in Guerrero State


Fig. 3, Topography Map showing the three concessions


5.0 Accessibility, Climate, Local Resources, Infrastructure and Physiography

From the city of Acapulco the project area is reached in approximately 6 hours if road conditions
are good (O’Dowd, 2009). From Acapulco one drives east on road MEX200 to the town of
Marquela (2 hours). From Marquela one drives north to Barranca del Panal, the last settlement
before the project which is located 4 kilometres to the east.

From Marquela to the project requires approximately 4 hours of a very sinuous and, and in some
parts, damaged road. The last portion of the road leading to the project area is in very bad
condition and a four wheel drive vehicle is recommended if the road is not upgraded. Access
might be a real challenge during the rainy season (August to October). The State government is
in the process of improving the road going from Xochiatenco up to the village of Barranca del
Panal.

Climate in the project area is temperate. Highs reach 35º C during the day while midnight lows
reach approximately 10º C. The area is heavily forested, mostly by pines. Lumber companies
are known to have been active in the area in the past. Roads in the area derive from that activity.
None is currently active

At the project, there is no electricity, telephone line or running water. Cellular phone service is
not available at this time on the property. The mine camp is represented by a few wooden shacks
which require a lot of work to make liveable. An old power line used to connect Barranca del
Panal to the mine site. A request has already been filed to re-establish this connection to the
federal electricity system. This process has not been initiated as of the date of this report. A
small river separates the campsite from most of the veins. A bridge will eventually have to be
built if heavy equipment has to be taken to the east side. An alternate road access could also be
evaluated and developed. Satellite communication equipment was used but the rugged terrain
made its use workable but unreliable.

Relief is very rugged. The base of the valley stands at approximately 1,400 metres ASL while
ridges reach 2,000 metres. The rugged terrain makes it very difficult to develop and maintain the
local infrastructure which is minimal at this point.


Fig. 4, San Javier Typical Topography, Mixtecapa River Looking Southwest

6.0 History

The State of Guerrero contains numerous precious metal deposits and mines. Within the State of
Guerrero, Goldcorp operates the Los Filos mines (60 MT, 0.991g/t Au), located in the Nukay
district, some 150 kilometres northwest of the project and Farallon Resources just started
production on the G-9 deposit (2.18 Mt, 3 g/t Au, 209 g/t Ag, 1.48% Cu, 1.32% Pb and 11% Zn)
located in the Campo Morado district some 210 kilometres to the northwest of the project as well
(these numbers are as of 2009).


Fig. 5, Map showing location of San Javier and other mineral deposits in Guerrero State

In the late 80’s and early 90’s, the family decided to develop some the known veins of the
property. A small 30 tpd flotation mill was constructed on the east side of the Mixtecapa River,
across and slightly upriver from the old campsite. The heavy material was then transported
through the river. According to Cesar Toledo who lived on site for 8 months at the time, the mill
operated at a rate of 25 tpd for at least 8 months. He estimates that at least 6,000 tonnes were
processed. This number could not be confirmed by members of the Larequi family at the time of
the field visits. It is clear that there are no good records of the historical production at the mine
and of the tonnage processed at the plant. Limited production from Veta Ancha (surface trench)
and Veta Cristo Rey (from a 80 metre long adit) were processed at the plant (possibly 6,000 to
7,000 tonnes, pers. Comm., Cesar Toledo) while material from Veta del Tajo (small pit near the
campsite and on the same side of the river as the campsite) was apparently hand-picked and
shipped directly to smelters in Mexico (250 tonnes, pers. Comm., Felix Larequi). According to
the Larequi’s, vein material was extracted from 7 different veins or portions of veins over the


years. Broad Oak cannot verify these production figures at this time. The historical estimate is
not being treated as a current estimate and the historical estimates should not be relied upon as a
current estimate.

Two holes were drilled by the Mexican government (Larequi, personal communication, 2012)
while the mine was operating. The results of that core drilling were apparently never given to
the owners. Geologist Cesar Toledo mentioned that he saw the core and confirms the presence
of mineralized structures. They were drilled down dip of Veta del Tajo and Veta Mixteco where
a stockwork zone is observed in the river. There is no known geology map of the property. Sr.
Cesar Toledo confirmed that he was the only ``geologist`` on site for the Larequi’s (8 months)
and that he was in charge of feeding the mill exclusively. All activities apparently ceased in
1993 because of low metal prices. The property has been idle from that time until 2009. Toledo
still acts as an experienced prospector and has a lot of knowledge of the local geology.
However, he does not have a P.Geo. designation and his formal training as a geologist is
unknown by ACA Howe or Broad Oak. He is not an independent Qualified Person in
accordance with Canadian securities commissions’ National Instrument 43-101 and as defined in
the CIM Standards on Mineral Resources and Reserves. In any event his work on the San Javier
property was carried out approximately 20 years prior to the implementation of National
Instrument 43-101 and therefore he is not familiar with the instrument or the CIM Standards.

In 2009, limited prospecting and sampling was performed, initially by Camsim, and then by First
Gold during the Company’s due diligence process. O’Dowd (2009) collected 12 samples from at
least 8 different veins. Two of the veins ended up being located outside of the San Javier
concession. Two of the samples were damaged during the shipment to the laboratory and were
eliminated because of possible contamination. Mr. O`Dowd is an independent Qualified Person
in accordance with Canadian securities commissions’ National Instrument 43-101 and as defined
in the CIM Standards on Mineral Resources and Reserves. No further work was carried out by
First Gold and the property was not acquired by that Company.

Assay Results from 2009 Due Diligence Sampling


7.0 Geological Setting and Mineralization

Regional geology is shown in Figure 6 (O’Dowd, 2009) and is a compilation of Mexican
government 1:250,000 scale geology maps E14-8-Chilpancingo (Consejo de Recurso Minerales,
1998) and E14-11-Acapulco (Consejo de Recurso Minerales, 1994). The project is found within
the southern portion of the precious metal belt of Mexico. Little is known about the geology of
the region. The area is part of the Mixteca Terrane. This structural province is considered to be
a pre-Mesozoic regionally metamorphosed nucleus of plutonic, volcanic and sedimentary
lithologies. The exposure of this basement reflects the uplift of the southern continental margin
of a cratonic nucleus. The presence of minor tin and tungsten on the property may be a
reflection of this metamorphosed continental basement. North-south shortening structures
originated during Laramide orogenesis that ended during Paleocene age. These may be reflected
in the project area as N-S and NE-SW property scale faults and lineaments. The terraine also
contains a relatively thin Cretaceous cover (Moran-Zenteno et al., 2007) of sediments (O’Dowd,
2009), as well as volcanic and sedimentary rocks of Tertiary age and granitic intrusions of
unknown age.

To date there is no detailed map of the San Javier project area. The 1:250,000 scale mapping of
the area covering the property suggests that is entirely underlain by intrusions of granitic
composition. The April 2012 fieldwork recognized two distinct rock units. To the south-west of
the Mixtecapa River is a highly weathered (kaolinized?) rock that has been considered
previously to be granite, and has been referred to in earlier reports as the Boracho Granite.
Examination of this unit by ACA Howe suggests that it may in fact be a rhyolite/dacite tuff, with
a minor flow component. To the north-east of the river is a much less weathered, much more
competent unit than its neighbour across the river to the southwest. It is more easily
recognizable as a granitic unit and is referred to in historical reports as the Maguey Granite.

The most recognized mineralized structures and the focus of mining and exploration to date
extend eastward from the Mixtecapa River into the Maguey Granite, and are best exposed on
Cerro Maguey. To date minor mineralization has also been observed southwest of the river in
the highly clay-altered (possibly) volcanic unit on Cerro Boracho. Past production at San Javier
comes from the Maguey Granite veins that extend from the river eastward a few hundreds of
metres from the contact. However, a review of previous reports suggests that those structures
extend several hundreds of metres further east. Typical alteration along the structures include
clay alteration (proximal and distal) and sericitization (proximal only).

In this region, all rock types but the Tertiary ones are mineralized, and it can be concluded that
the epithermal system was active in the early-mid Tertiary. Typically in Mexico deep intrusive
activity during the Eocene and early Oligocene epoch was followed during the cooling event by
a collapse event and the emplacement of mineralized epithermal systems. In San Javier, it
appears that mineralized structures develop in the more brittle of the two granites of the region.


Fig. 6, Regional Geology


Fig. 7, Possible felsic crystal tuff – formally Boracho Granite

Fig. 8, Maguey Granite


MINERALIZATION

To date, approximately ten veins have been discovered east of the Mixtecapa River and only one
lies west of the river. Seven of those have seen some small scale production. Because of the
vegetation cover, the veins are poorly exposed along the slopes of the mountainous terrain
forming the property. They are better exposed along creek beds. For this reason, it is quite
difficult to establish their extent
.
The veins east of Mixtecapa River range from a minimum 50 centimetres to a maximum of 3-4
metres (e.g. Veta Ancha). They mostly strike in an E-W direction with a moderate dip to the
south (approx. 45o ). However, diverging strikes and dips and cross cutting relationships were
observed. Pinch and swell structures were also observed indicating that mineralized shoots are
to be expected.

Stockwork structures appear to be present in some areas. The two drill holes completed near
Veta Mixteco seem to have targeted such an area. The area west of Mixtecapa River contains an
approximate 85 metre vertical section of such coarse (1.8 metres) vein to fine (2 centimetres)
mineralized stockwork. It is probable that systematic mapping and stripping will uncover more
mineralization of both types on the project.

8.0 Deposit Types

The polymetallic mineralization at San Javier (galena, arsenopyrite, pyrite, acanthite, sphalerite,
chalcopyrite) is related to epithermal activity during the Tertiary era. This type of mineralization
is found all along the metallogenic belt of Mexico (Sierra Madre, 2,000 km). It hosts some of
the most famous silver districts in the world (Fresnillo, Guanajuato and others). Typically, the
mineralization can be found in extensive vein systems, in stockwork, in pipes or even
disseminated (Camprubi and Albinson, 2006). All rock types can host the mineralization but
more ductile units are often favoured. Grades are extremely variable. Disseminated deposits can
be very low grade (Peñasquito, 0.5 g/t Au) while bonanza grades are often observed in veins and
pipes (Fresnillo, + 1000 g/t Ag). Their metallogeny is also quite variable. Some are typically
precious metal rich (Au>Ag or Ag>Au) while others are richer in base metals.

9.0 Exploration

Vendome’s 2012 (spring) exploration program was conducted and managed by ACA Howe
International Ltd. ACA Howe’s exploration activities involved satellite imagery analysis and
interpretation, an extensive rock and soil sampling program on the San Javier Property, with
focus on the western side of the concession as the Company is in the process of finalizing a
surface access agreement with the local community. The satellite imagery (Quickbird) work was
carried out to outline property scale structures and to separate by spectral color and intensity
changes areas of strong clay and oxide alteration that could be related to hydrothermal activity.
It was also used to attempt to recognize changes in lithology. The geochemical program
primarily focused on soil, channel, grab and stream sediment sampling, plus limited prospecting.


In addition, grab samples were taken from veins on both the east and west side of the river in
areas that were previously explored in order to confirm assay values reported from previous
studies. Two water samples from Mixtecapa River were also taken.

SATELLITE (QUICKBIRD) IMAGERY

The regional view provided by the Quickbird image (Figure 9, A.C.A. Howe, 2012) shows
several linear structures that are interpreted as regional fault systems. These are probably deep-
penetrating and would allow the lateral and upward movement of hydrothermal mineralizing
fluids. Dark green patches represent basement complex rocks. These appear as “windows”
through the more mottled buff/medium green coloured terrain which may be volcanic, mainly
tuffaceous cover. Cross-hatched areas are steep slopes to the opposite more gentle NE and E dip
slopes to those volcanics.

Figure 10 shows the results of spectral imagery analysis. In this case this analysis was used to
show the presence of kaolinite (green and blue) and the presence of alunite (yellow and red).
Alunite is generally considered to represent the alteration of plagioclase feldspar of volcanic
rocks while kaolinite is the more general alteration product of feldspar. A narrow wedge-shaped
alunite alteration zone is found N and NNW of the San Javier property, and as small patches at
Tajo, Ancha and several other sites surrounding the project. The linear nature of the main zone
suggests it is related to a major NNE-SSW regional structure. Interpretation has also outlined a
NNE trending zone of enhanced silicification and (Fe) oxidation. Note that this
alunite/silicification/Fe oxidation covers the NW quarter of the property.

In the immediate area of the San Javier property (Figure 11) there is a color change that reflects
the compositional and textural difference between the two main host rocks described under
Regional Geology. As shown on the figure this includes the Maguey Granite as a dark greenish
patch surrounded by a mottled buff and lighter green region covering the majority of the ground
in and around the project. This represents a felsic volcanic tuff. Several other dark green
patches occur outside the project. All may represent windows through younger units to the
metamorphic basement. Note the steep vs. gentle slopes of hills. The steepness may be due to
slumping of the tuffs or their sedimentary equivalents while the shallow slope may represent an
approximate paleosurface and dipslope.


Fig. 9, Satellite Imagery Regional Interpretation


Fig. 10, Satellite Imagery, Interpretated Alteration Zones


Fig. 11, Property Geology from Satellite Imagery


SOIL SAMPLING

Soil grids were established and figures 12-16 show the results. The upper part of the grid
showed only weakly scattered (maximum 7 g/t) silver values. Arsenic showed high values over
the south half of the grid (maximum 5,850 ppm) while lead shows a similar anomaly (maximum
5,220 ppm) in the south half, but it provides a NNE trend, suggesting a dip (vein is going deeper)
in this direction. A similar, though weaker, response was seen in zinc with a maximum of 200
ppm. Strike/dip measurements of veins in the roadcuts show a similar NE dip direction. Highest
elevation here is 1,382 metres above sea level.

The lower part of the grid is set out on the east-facing slope between the Upper and Lower Tajo
access roads. Assay results suggest two weak anomalies in silver values, with a maximum of
16.1 ppm. Arsenic anomalies are focused in the south half of the grid and produce a broad NNE
trend. The maximum value was 8,130 ppm. Lead showed a similar broad anomaly in the south
grid area, giving a maximum value of 9,180 ppm. A single sample in the NW (3130 ppm),
coupled with a weaker aresenic anomaly from the same sample, suggests a second small parallel
NNE trend. Zinc values emphasize both trends and suggest a third parallel trend. These all
indicate the probability of three separate veins coming to surface along these NNE trends. A
broad west side and less extensive east side may indicate a shallow to moderate west dip to the
veins. Note that although the road at the south end has been disturbed material has probably not
been moved more than a few meters.


Fig. 12, Silver in Soils


Fig. 13, Arsenic in Soils


Fig. 14, Copper in Soils


Fig. 15, Lead in Soils


Fig. 16, Zinc in Soils


ROAD CHIP CHANNEL SAMPLING

Three hundred and sixty-six channel samples were obtained along the Upper and Lower Tajo
roads between April 4 and April 16, 2012 (Figures 17-19). Vertical channel samples were
collected from the outcrops along the road and horizontal channel samples crossed over the road.
In general, the rock is so highly altered in this area that the use of a rock saw was not necessary
for sample collection. Vertical channel samples were spaced 5 metres apart and gathered over
continuous 1-metre intervals, as high as reach allowed (typically 1-3 metres). The horizontal
channels also had 5 metre spacings and were sampled continuously, but comprised of 2 metre
sample intervals. Not all horizontal channel samples were in situ, particularly along Lower Tajo
Road; however, the material appeared local and very near to source and should therefore have no
effect on geochemical results. This extensively sampled area links with both soil grids, creating
one large continuous sample zone immediately west of the river above Veta Tajo. The samples
were sent to SGS Laboratory in Durango for fire assay and ICP analysis.

Sampling focussed on the Veta Tajo area located 300 metres southwest of the historical San
Javier mine workings. It is believed the Veta Tajo is a previously unrecognized, unexplored and
unexploited area of significant visible stockwork quartz veining that spans an 80 to 100 metre
vertical rise in the west bank of the river valley that transects the central property area.

Quartz veining in the Veta Tajo is stacked, horizontal to shallow-dipping and consists of:
a set of 0.8-1 metre thick veins dipping 40-60° to the east
a second set of 25-40 centimetre thick veins dipping 25-35°
a third set of 2-5 centimetre thick veins dipping 0 to 15º

Select weighted averages for silver concentration over continuous chip sample lengths in the
Veta Tajo are as follows: (channel lengths are not true widths)
Vein Silver Channel
Sample No. Easting* Northing*
Orientation (g/tonne) Length (m)
KGC023-025 vertical 222 3 540804.4 1894954
KGC053 vertical 616 1 540831.1 1894940
KGC091-99 horizontal 239.5 18 540784.4 1894966
KGC0314-322 horizontal 471.6 16 540817.5 1894925
* - approximate center of chip channel using UTM WGS8, Zone 14Q

Veining appears to be associated with east-west structures cross-cutting a host rock previously
identified as "old granite", which ACA Howe has re-interpreted as strongly silicified felsic
volcaniclastics. ACA Howe's field work also indicates that veining extends into areas north and
south of Veta Tajo. Vendome management is extremely encouraged by these chip results in that
the potential for bulk silver mineralization in wall rock, in addition to high grade narrow vein
mineralization has been confirmed.


Fig. 17, Silver in Chip Samples


Fig. 18, Arsenic in Chip Samples


Fig. 19, Lead in Chip Samples


STREAM SEDIMENT SAMPLING

On April 16, 2012 a total of 14 stream sediment samples were collected by Howe personnel
along the Mixtecapa River (Figure 20). Sampling began at the Veta Ancha mill area and
followed the Mixtecapa River to the north boundary of the San Javier concession. Stream
sediments were collected approximately every 50 metres along the western side of the river.
There was limited outcrop bordering the river along this 500 metre stretch; small to very large
boulders occupied the river instead. The fourteenth sample, KGS-14, was taken from a nearly
dried up tributary by Veta Ancha approximately 40 metres inward from the Mixtecapa River.
The sediment consisted of coarse sand here, as opposed to the fine silt and clay sediment in
samples KGS-01 to KGS-13. These samples were sent to SGS Laboratory for ICP analysis.

None of the samples along the Mixtecapa River showed anomalous values. The sample taken
from the dried tributary near Veta Ancha (KGS-14) showed 6 ppm Ag, 180 ppm As, 430 ppm Pb
and 518 ppm Zn, well above any of the other sample results. It is unknown at this time whether
this is the result of sampling of mill tailings or if it is related to the Veta Ancha itself.

Fig. 20, Stream Sediment Sample Sites

SELECT ROCK SAMPLING

Between April 2 and April 17, 2012 limited prospecting was done around the property, focusing
on the western side of the Mixtecapa River. Grab samples (KG-001 to KG-034 and DB-01 to


DB-12) were collected from various veins and mineralized or highly altered host rock. Samples
were also taken from one of the old adits located upstream from Veta Tajo (KG-022 to KG-024)
and from the ore pile (KG-028 to KG-031).

Results of April 2012 Select Rock Sampling (UTMs are in WGS84 Zone 14Q format)

Sample UTM E UTM N Ag As Pb Zn
m m ppm ppm ppm ppm
KG-01 540522 1893981 1818 49200 4000 811
KG-02 540520 1893978 135 28200 4470 3965
KG-03 540499 1893896 72 20900 >10000 4894
KG-04 540797 1894954 304 20800 >10000 113
KG-05 541269 1895435 32 170 2090 882
KG-06 541151 1895442 325 1900 3450 2626
KG-07 541139 1895063 17 970 1950 585
KG-08 541008 1894911 18 1340 970 1205
KG-09 540862 1894870 559 27600 >10000 >10000
KG-10 540739 1895027 11 130 80 70
KG-11 540777 1894969 574 18300 7840 206
KG-12 540785 1894959 115 9370 5160 193
KG-13 540775 1894957 4352 29300 >10000 361
KG-14 540777 1894948 2907 32300 >10000 488
KG-15 540790 1894933 792 18800 5770 146
KG-16 540789 1894985 1063 24600 3880 171
KG-17 540791 1894975 1373 22600 9230 85
KG-18 540797 1894961 573 7110 6100 507
KG-19 540799 1894951 572 12400 8660 129
KG-20 Standard 6 440 440 >10000
KG-21 540802 1894935 548 13100 6420 229
KG-22 540866 1894879 <2 100 30 30
KG-23 540866 1894879 3 130 40 42
KG-24 540866 1894879 101 28100 7320 3805
KG-25 540880 1894927 59.1 70 220 103
KG-26 540880 1894927 73.4 49500 6570 171
KG-27 540880 1894927 113 37100 8760 278
KG-28 540768 1894841 263 48300 8880 >10000
KG-29 540768 1894841 19.2 20300 2730 5856
KG-30 540768 1894841 35.7 20600 2840 3915
KG-31 540768 1894841 158 11100 3860 7511
KG-32 540418 1895249 <2 210 100 134
KG-33 540350 1895403 <2 80 20 22
KG-34 Blank <2 100 100 193


April 2012 Select DB Rock Sampling (UTMs are in WGS84, Zone 14Q format)

Sample UTM E UTM N Ag As Pb Zn
m m ppm ppm ppm ppm
DB-01 540872 1894917 2334 11500 9090 95
DB-02 540871 1894920 442 23600 6020 112
DB-03 540847 1894908 2572 13900 12300 112
DB-04 35 m Az 060 Same vein as DB-03 898 14700 4170 82
from DB-03
DB-05 540886 1895074 240 2310 2560 83
DB-06 540863 1894952 48.7 4370 2250 123
DB-07 4 m uproad from 235 13300 8430 97
540863 E/1894952 N
DB-08 13 m uproad Same vein as DB-07 in 6672 25500 4580 77
from DB-07 Floor at base of roadcut
DB-09 27 m uproad Same vein as DB-07 in 7212 32400 13200 384
from DB-08 Floor at base of roadcut
DB-10 540871 1894961 1510 22600 4350 89
DB-11 540744 1894935 535 8760 2020 287
DB-12 540755 1894876 158 17200 6300 59

10.0 Drilling

It is reported by the owners of the property that Mexican government geologists drilled two holes
within the project. The owners were not given a copy of the results and neither the Company,
ACA Howe, or Broad Oak have to date found a copy of those results.

No drilling has been carried out on these Properties by the current owners or joint venture
partners.

11.0 Sampling Method, Analyses and Security

Sampling Methods and Approach
Representative continuous chip samples and most selected grab samples were removed from the
outcrop surface by chipping with a geological hammer. The focus of the sampling was mainly
on altered rock and vein material. The chip samples collected from vertical outcrops were taken
over 1 metre intervals and each channel was spaced 5 metres apart. Those samples collected
over horizontal outcrops were taken over 2 metre intervals and also spaced 5 metres apart. All
rock samples were placed in labelled plastic bags and/or cloth bags and sealed.

Soil samples were collected using a trowel by first removing all vegetation and organic matter.
The soil samples were placed in labelled kraft paper envelopes and sealed. The 63 samples from
Soil Grid A were collected every 10 metres, along lines that were spaced 25 metres apart. Soil
Grid B contains 127 samples that were collected every 10 metres, along lines spaced 10 metres
apart.


The stream sediment samples were collected approximately every 50 meters along Mixtecapa
River, but more specifically, in areas of reduced flow rates where settling of higher density
(heavier) material was likely to occur. Samples were gathered using a trowel and then squeezed
by hand to eliminate the water. They were placed in labelled kraft paper soil sample envelopes
and left out in the sun to dry.

GPS locations of the grids, stream sediment, water and select rock samples were recorded
utilizing a handheld GPS receiver. The sample number, description, assay results and location
(UTM coordinates) were then compiled in a Microsoft Excel spreadsheet.

It is Broad Oak’s opinion that all of the sampling was carried out according to industry standards
and the samples are representative of mineralization at the Project.

A total of 618 samples (including field duplicates, blanks and standards) of rock, soil, stream
sediment and water were collected during the April 2012 exploration program. Of these, 366
were rock chip samples, 46 were rock select (grab) samples, 190 were soil samples, 14 were
stream sediment samples and 2 were water samples. All of these samples were sent to SGS
Laboratory in Durango, Mexico for geochemical analyses.

SGS Durango is an internationally recognized independent ISO-certified lab; it conforms to the
requirements of the ISO/IEC 17025:2005 standard for the General Requirements for the
Competence of Testing and Calibration Laboratories. It is a Standards Council of Canada
Accredited Laboratory (No. 657) and conforms to requirements of CAN−P−1579 (Mineral
Analysis) and CAN−P−4E. Its scope of accreditation includes fire assay with Atomic
Absorption Spectrometry (AAS) and gravimetric analysis for gold and silver; aqua regia
digestion, strong acid digestion and peroxide fusion by Inductively Coupled Plasma Optical
Emission Spectrometry (ICP-OES), and 3 acid digest for Silver by AAS and titration methods
for concentrates.

Methods used in the analysis of the San Javier samples included those described below. Based on
historical results and budget allowed for assay costs no analysis was requested for Au

Sample Security
All chip and soil samples were collected by a 3-man sampling crew under the supervision of
Karen Grey, GIT, with regular review by Dr. Duncan Bain, P.Geo. A numbered sample tag was
placed in each bag and the number was also written with waterproof marker on the outside. Each
bag was then closed with plastic zip ties. All samples were placed in plastic pails (15 to 20 per
pail) with snap-lock lids. The sample batch was written on each pail. All samples were driven to
the lab by a temporary employee of Camsim. He had no list of the samples nor was he informed
where individual samples were taken from. He was under the supervision of a ACA Howe QP.

Sample Preparation
Method PRP85 was used to prepare rock, soil and stream sediment samples. Samples of <1.2 kg
weight were dried, fine pulverised to a nominal 75μm using bowl-and-puck equipment. No
preparation was carried out for the water samples.


Analytical Procedures
ICP-40B was used to analyse 40 major and minor elements, including major base metals and
silver. This method involved Induced Coupled Plasma Mass Spectrometry (ICP-MS). In plasma
mass spectroscopy, the inductively coupled argon plasma (ICP) is used as an excitation source
for the elements of interest. The plasma in ICP-MS is used to generate ions that are then
introduced to the mass spectrometer. These ions are then separated and collected according to
their mass to charge ratios. The constituents of an unknown sample can then be identified and
measured. ICP-MS offers extremely high sensitivity to a wide range of elements. It is a multi-
element analytical technique capable of determining an extremely wide range of elements to very
low detection limits (typically sub ppb). Any samples with Ag values greater than 10,000 ppm
(10 g/T) were re-analyzed using method AAS-21B and/or FAG313. Any base metals with values
greater than 10,000 ppm (1.00%) were re-analyzed using method ICP90Q.

AAS-21B is used to measure samples with greater than 10,000 ppm (10 g/T) Ag. It has an
analysis range from 0.3 g/t to 300 g/t. It uses a 2g sample that undergoes 3-acid Digest with an
Atomic Absorption Finish (AA).

ICP90Q is used to achieve suitable precision and accuracy for ore grade base metals with values
greater than 10,000 ppm (1.00%). This ore-grade analysis is typically performed using a sodium
peroxide fusion and ICP-AES (Atomic Absorption Spectroscopy) analyses.

FAG313. This method is used to achieve high precision for Ag-rich rock samples with
anticipated values greater than 5 g/t. It involves a fire assay and gravimetric finish. Fire assaying
involves the mixture of sample and an appropriate flux that is then melted in a crucible. Upon
cooling the “slag” is removed. Various chemicals are then added to separate the various metals
in the remaining bead. These are weighed individually to give an assay value. Gravimetric
finish is a method of weighing the specific bead with a highly sensitive balance to provide more
precision to the resulting assay value.


12.0 Data Verification

Fig. 21, Sample Locations July 6, 7 2010 Visit

Broad Oak Samples taken on the 6 and 7 of July 2010 from the Vendome Sam Javier
Polymetallic Project, State of Guerrero, Mexico.

All the samples were taken as grab samples from the outcropping veins or dump site.
Datum WGS 84

Vien on Road
BOA 1 UTM Coordinates 14 Q E 540741 N 1894855
8,299 g/t silver 834 ppm copper 6250 ppm lead 615 ppm zinc

San Javier Old Dump
411 g/t silver 2,080 ppm copper >10,000 ppm lead >10,000 ppm zinc

Sample 1 Adit
15,042 g/t silver 6,220 ppm copper >2,270 ppm lead >10,000 ppm zinc


Sample 2 Adit higher up
109 g/t silver 558 ppm copper >10,000 ppm lead >2,310 ppm zinc

Veinlets in river bed
204 g/t silver 1,600 ppm copper >10,000 ppm lead >2,340 ppm zinc

Fig. 22, Grab Sample locations 5, 6 December 2011 Visit

Broad Oak Samples taken on the 5 and 6 of December, 2011 from the Vendome San Javier
Polymetallic Project, State of Guerrero, Mexico.

All the samples were taken as grab samples from the outcropping veins.
Datum WGS 84

1,277 g/t silver 1,590 ppm copper 2.39% lead 2.51% zinc

242 g/t silver 122 ppm copper 1.77% lead


49.7 g/t silver 21 ppm copper

1,384 g/t silver 176 ppm copper

38.4 g/t silver 404 ppm copper

105 g/t silver 281 ppm copper 1.69% lead

657 g/t silver 8,500 ppm copper 7.32% lead 4.18% zinc

54.1 g/t silver 236 ppm copper 1.4% lead

These grab samples were assayed at SGS Durango. It is an internationally recognized
independent ISO-certified lab; it conforms to the requirements of the ISO/IEC 17025:2005
standard for the General Requirements for the Competence of Testing and Calibration
Laboratories.

Broad Oak believes that these samples indicate that there is high grade mineralization on the
property and that they confirm the exploration program results reported by ACA Howe.

13.0 Mineral Processing and Metallurgical Testing

In the early 1980’s, a 30-ton per day mill was set up on the property. The remains of this plant
can still be viewed. There are no reliable production records available. To the authors’
knowledge, no records of metallurgical testing during that time exist, and no such work has been
carried out since then.

14.0 Mineral Resource Estimates

There are no NI 43-101 compliant resources on this property.

15.0 Mineral Reserve Estimates

There are no NI 43-101 compliant reserves on this property.


16.0 Mining Methods

Not Applicable.

17.0 Recovery Methods

Not Applicable.

18.0 Project Infrastructure

The project is in a remote area and access is difficult. Any assistance of a technical nature has to
be brought into the area, and appropriate accommodations provided. There is ample labour in
the surrounding villages and this is readily available as there is very little employment in the
area.

19.0 Market Studies and Contracts

Not Applicable.

20.0 Environmental Studies, Permitting and Social or Community Impact

The only possible environmental issue relates to the small historic mill site. There is a small
tailings impoundment that may need to be remedied, but at present there are no requirements for
this to be done. Water testing did not indicate at the time of testing that these tailings are
leaching any deleterious material.

21.0 Capital and Operating Costs

Not Applicable.

22.0 Economic Analysis

Not Applicable.


23.0 Adjacent Properties

Fig. 23, The San Javier, La Diana, and San Miquel Properties

Vendome owns most of the adjoining properties and apart from the following interpretation of
satellite imagery there has been no exploration carried out on these properties. This map was
compiled by Howe.


Fig. 24, Satellite Image Interpretation Map


24.0 Other Relevant Data and Information

There is no other relevant data and information.

25.0 Interpretation and Conclusions

The April 2012 Phase 1 exploration program carried out for Vendome by ACA Howe confirmed
the presence of highly anomalous assay values in silver (up to several thousand g/t in select
samples), arsenic, lead and to a lesser extent Zinc, as had been described in historical reports on
the San Javier project. Most of these reports had focused on the mineralized veins east of
Mixtecapa River. Because of local community concerns about mineral exploration east of the
river, only a single day of the April 2012 program was spent examining these veins and taking
select samples to confirm assay values described previously. That visit indicated that there are
several sub-parallel generally east-striking and south dipping mineralized veins. Subject to more
detailed examination, these veins appear to be hosted by a relatively fresh-looking unit referred
to as the Maguey Granite (in older literature referred to as the Young Granite). Regional
geology refers to the area as being underlain by Mixteca Terrain, a mix of pre-Mesozoic
plutonic, volcanic and sedimentary rocks regionally metamorphosed by the Laramide (and
older?) orogeny. However, the relatively unaltered textures and composition of this granite and
younger mafic dykes intruding it suggest it is more likely post-Laramide (post-Cretaceous) in
age. Veining in that area would then also be younger than that intrusion. The quartz vein-host
rock, with no carbonate, plus the silver-arsenic-lead but low zinc and even lesser copper
indicates that current position is at moderate depth in an epithermal system. High arsenic shows
that hydrothermal fluids have leached a thick section of crustal material (the Mixteca Terrane).
This mineralized system is related to regional scale structures that penetrate that terrane to great
depth. It is probable that additional veins are present in proximity to other regional structures on
and around the San Javier property.

Because of local political issues most of the recently completed work concentrated on known
mineralization from the Tajo Vein westward to the western property boundary. Here the host
rock was a moderately to strongly clay-altered buff- to light brown to orange-pink host rock that,
although previously considered to be a granitic rock, is considered by Dr. Bain (Howe) to be a
lithic and crystal tuff of rhyolite to dacite (felsic) composition. This unit is thought to be post-
Maguey Granite in age. However the mineralizing event is probably the same on both sides of
the river. Sulphide and silver minerals are the same, as are the ranges in assay values. Gangue
mineral in the veins and stockwork are both quartz with no carbonate. In the west this
mineralization is recognized in a much more stockwork type pattern compared to the east where
individual thicker veins with much less stockwork are more prevalent. Zones of silicification are
more easily recognized in the west.

It is suggested that the Maguey Granite was injected through the Mixteca Terrane after the
Laramide Orogeny, so as late as Tertiary time. That surface was eroded down to expose the
granite. Following this felsic volcanism, including ash clouds, ashflows and minor rhyolite
flows occurred in the region. A glassy brittle horizon may have been present at the base. The
porous and permeable nature of the tuff would easily allow the movement of hydrothermal fluids


along its base, especially against an impermeable surface such as the Maguey Granite. That
basal zone had “crackled”, either from a possible glassy base or because there was an initial
phase of hydrothermal fluid movement that precipitated only silica. That “crackling” created
numerous small-scale (2 centimetre to 1.8 metre) flat to low-angle stockwork veinlets and rare
small veins. West of the river mineralization can be projected to at least the elevation of
Mixtecapa River (1,308 metres) and as high as the surface of Soil Grid (1,382 metres), an
elevation difference and therefore a known vertical mineralized zone of a minimum of 74 metres
thick. Dip direction may be influenced by the original slope of the granite basement, allowing
NE, W and NW dip to the stockwork and veins west of the river. Concurrent or a later phase
fluid movement remobilized or carried into this stockwork the same metals (Ag-As-Pb-(Zn)-
(Cu)) and sulphur as those seen in the Maguey Granite. The acidic nature of the fluid caused the
moderate to strong clay alteration of the feldspars of the volcanic pile but much less in the
feldspars of the Maguey Granite. Veining and mineralization in the granite may reflect a greater
depth in the hydrothermal system. This interpretation would require that volcanics also be
deposited east of the river at the same time as those to the west but have since been eroded,
possibly because of uplift of the east side was along a NE fault along the river following the
mineralizing event. Insufficient sampling has been done on the east side to show if there is
increase in Cu values which would suggest that veining there is deeper in the hydrothermal
system. Little analysis has been done for gold. An increase in one or both elements would be a
strong indicator of increased depth in the system.


The following figures show the vein locations on the San Javier property as identified to date.

Fig. 25, Vein Locations San Javier Property


Fig. 26, Vein Locations North Portion of San Javier Property

Fig. 27, Vein Locations South Portion of San Javier Property


26.0 Recommendations

Geoffrey S. Carter, the Qualified Person preparing this Technical Report, believes that the
character of Vendome Resources Corp. San Javier, La Diana and Fiscal 2012 Projects are of
sufficient merit to justify the following exploration program over the next 12-24 months.

It is recommended that a 2 Phase program be initiated on the Vendome Properties to provide
more detail to the silver, gold and base metal potential of the property and the areas surrounding
it. Budget estimates and work programs are outlined below. Phase 2 is contingent upon the
results of Phase 1.

Phase 1

The Phase 1 program should consist of detailed mapping of the known veins and their host rocks
east of the Mixtecapa River, as well as a few days of mapping and prospecting in the northwest
quarter of the property, to look for evidence of Tajo Zone veining, alteration and mineralization.
An IP/Resistivity ground geophysical survey would not be effective on the flattish veining west
of the river. However, it would be useful in trying to trace the continuity of more moderate and
steeply dipping mineralized veins such as Veta Ancha east of the river. It would also be used to
assist in the selection of drill targets on that side. Based on the Aster satellite imagery and
apparent disposition of hydrothermal alteration and structure, La Diana and San Miquel
concessions may host mineralization similar to that at San Javier and consequently with it the
possibility of multiple prospects and occurrences across the properties. It is recommended that
an airborne magnetic, EM and radiometric survey together with a regional stream sediment
geochemistry survey be conducted across the properties in order to identify additional veining
and mineralization.

The Tajo Road area has been geochemically sampled in detail. An 85 metre deep stockwork and
vein zone is present there. Both the Veta Ancha and Tajo road area represent immediate targets
for diamond drill testing and it is recommended that the continuity, vertical density and variation
in width of veining in the two areas drill tested as part of the Phase 1 work.


Proposed Phase 1 Budget

Item $USD

MAPPING AND SAMPLING

Mapping and Sampling 40,400

REGIONAL STREAM SED GEOCHEMISTRY

Geological Staff 29,200
Assays 15,000
Helicopter Support 150,000
Purchase Camp 100,000
Camp Operation and Transportation 50,400
Reports 50,000
GEOPHYSICS

IP/Resistivity survey 50,000
Airborne EM/magnetic/radiometric survey – San Javier/Diana 300,000
Concessions – 100m spacings = total 3,000 line-km
DRILLING

Diamond Drilling 8,000 metres 1,600,000
Assays and sample preparation 260,000

SUB TOTAL 2,792,000
Contingencies 15% 418,800
TOTAL PHASE 1 PROGRAM 3,210,800


Phase 2
Assuming the results from phase 1 support a second phase, phase 2 would continue work on the
large land position and drill any further targets identified in phase 1.

Proposed Phase 2 Budget

Item $USD
REGIONAL FOLLOW UP MAPPING, STREAM
SEDIMENT, SOIL GEOCHEMISTRY

Assays 60,000
Helicopter 112,500

DRILLING

Diamond drilling, 10,000 metres 2,000,000
Assays 260,000
Camp Operation and Transportation 41,400
Reports 35,000

SUB TOTAL 2,717.000
Contingencies at 15% 407,550
TOTAL PHASE 2 PROGRAM 3,124,550

The total of phase 1 and phase 2 is US$6,335,350


27.0 References

Report on the exploration on the San Javier Silver Project, Barranca Panal Area, Central Guerrero State,
Southwestern Mexico. Vendome Resources Corp.. A.C.A. Howe International Limited, Toronto,
Ontario, Canada. Dr. Duncan Bain, P. Geo., Felix Lee, P. Geo., Karen Grey, B. Sc., G.I.T.,
June/July 2012.

Satellite Image Interpretation of the San Javier and Diana Properties, the State of Guerrero, Mexico, for
Vendome Resources Corp., April 2012

Consejo De Recursos Minerales, 1998, Carta Geologico-Minera Chilpancingo, E14-8, Guerrero,
Oaxaca and Puebla

Consejo De Recursos Minerales, 1998, Carta Geologico-Minera Acapulco, E14-11, Guerrero,
Oaxaca and Puebla

Moran-Zentano et al., 2007

O`Dowd, 2009


CONSENT OF AUTHOR

To: securities commissions and exchanges where filed

I, Geoffrey S. Carter, do hereby consent to the filing of the written disclosure of the Technical
Report titled Polymetallic Resources on the San Javier, La Diana, and Fiscal 2012 Properties and
dated October 17, 2012 (the Technical Report) related these projects and any extracts from or a
summary of the Technical Report in the material change report of Vendome Resources Corp. and
to the filing of the Technical Report with the securities regulatory authorities referred to above.

I also certify that I have read the written disclosure being filed and that it fairly and accurately
represents the information in the Technical Report that supports the disclosure of Vendome
Resources Corp..

Dated the 17th Day of October, 2012

Seal or Stamp

Geoffrey S. Carter

Printed name of Geoffrey S. Carter, P. Eng

Copyright of Broad Oak Associates (A Division of 930531 Ontario Limited), Head Office: 365 Bay Street, Suite 304, Toronto, Ontario, Canada,
M5H 2V1


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