Report of Diamond Drilling Program for Explorers

I
REPORT OF DIAMOND DRILLING PROGRAM FOR
EXPLORERS ALLIANCE CORPORATION
ENID CREEK PROJECT
LOVELAND TOWNSHIP
PORCUPINE MINING DIVISION
Submitted by Lionel Bonhomme
May 24, 2011
Contents
Page 1:
Introduction, Location, Regional & Local Geology
Page 2:
Previous Work
Page 3:
Certificate
Page 4:
Claim Sketch
Page 5:
Regional Location
Page 6:
EL-25-0BXX Drill Hole Plan
Page 7:
EL-25-0BXX Drill Hole Section
Pages 9-:
EL-25-0BXX Core Log
1
Introduction:
The Enid Creek project is located in south east Loveland Township,
approximately 14km north of the past producing KamKotia Mine. International
Explorers & Prospectors Inc conducted a one drill hole program, totaling 63m by
extending a previous drill hole that had not reached a favourable contact. The
contractor was Colbert Drilling (167 Jury Lane, Timmins) with a start date of May
17, 2011 to May 24, 2011. The layout and location was performed by Peter
Colbert, who located the previous casing. Wayne Corstorphine was retained to
log and describe the drill hole. The drill hole collar for EL25-08X is 50+00E,
10+175N, 452282mE, 5383225mN, Nad 27 zone 17, 270° azimuth, with a dip of
-70°. Water for the drilling was obtained from a low marsh nearby.
Location:
The property owned by International Explorers & Prospectors Inc in
Loveland Township, plan M-0293 consists of 10 unpatented contiguous units.
The property can be accessed by paved highway 101 west from the City-of
Timmins, then following the Malette Logging road for 20km and turning onto
Winter Lake Road for 8km, then 1.5km on a previously used drill road
constructed by a logging company. A four wheel drive vehicle is required to
access the drill site. Travel time to the drill site is approximately 90min.
Regional Geology:
The area is situated at the west end of the Abitibi Greenstone Belt,
which consists of Archean meta sediments and felsic to mafic volcanics, intruded
granitic and mafic intrusive bodies. A description of the geology is reported by
Ferguson (1944), Middleton (1972), Pyke (1970), Hart (1983), Barrie (1990) and
Ayer (2005).
Local Geology:
The property has a large outcrop of mafic intrusive gabbro in
contact with the andesite and large blocks of andesite can be observed
before the final andesite contact and disseminations of sulphides are also
observed before the contact where sulphides are observed in massive form
over several centimeters. This outcrop confirms the fact that tens of meters
of andesite can be observed before the key contact.
2
Previous Work:
1951-1956 Hollinger mines geophysics drilling programs.
1988-1989 Falconbridge geophysical and diamond drill program
1994-1995 Westminer Geophysical, compilation and diamond drill
2000- 2010 Explorers Alliance Corporation Diamond Drill programs.
3
Certificate
I, Lionel Bon hom me, hereby certify that,
I am a member of the PDAC of Canada and Porcupine group,
I am the holder of a valid prospector's license for the province of Ontario,
I am a member of the Geological Association of Canada,
I have been actively involved in exploration since 1964,
My spouse is a shareholder of International Explorers & Prospectors Inc.
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DRILL HOLE• EL25-08XX <2nd
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EL25-08XX
PROSPECTORS INC
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306.00
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PROJECT: ENID CREEK (LOVELAND>
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INTERNATIONAL EXPLORERS
g,...a;"f:>ct
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ORIGINAL EOH 106.0n <2008)
FIRST EXTENSION to 246.0n <2010)
DATE I 11/05/23
SCALE1 111500
r');-,
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1/r. Ontario
Ministry of
Northern Development
and Mines
Ministere du
Developpement du Nord
et des Mines
Drill Log
Journal de forage
Under section 8 of the Mining Act, this information is used to maintain a public record. I Aux termes de I' article 8 de Ia Loi sur les mines, ces renseignements serviront
Hole ID I Forage no
Claim No. I No de concession miniere
Township/Area I Canton
EL25-08XX (second extension)
PI037161
Loveland
Name of Land Holder I No, de
Azimuth
International Explorers & Prospectors
Inc.
270
Drilling Company I Compagnie de forage
Logged by (print) I
lnscrit par (ecrire en lettres moulees)
Colbert Exploration & Drilling Co.
Dip I lnclinaison
°
-70
End of Hole (m) I
fin de forage (m)
°
306.0m
W Corstorphine
Date Hole Started (yyyylmmldd) I
Date de commencement du
forage (aaaalmmljj)
Date Completed (yyyylmmlddJ I
Date d'achevement (aaaalmm!JJJ
2011/05/18
2011/05/21
Footage/Avancement
From/De
BQ
Date Logged (yyyylmmldd) I
Date d'inscription au journal
I
of I de
3
a tenir a jour les dossiers publics.
DRILL HOLE COLLAR LOCATION CO-ORDINATES I
COORDONNEES DU COLLIER DE TROU DE FORAGE
Overburden Depth I
profondeur des mortsterrains
UTM I MTU
Latitude I Longitude
degrees/minutes/seconds or decimal values
degreslminuteslsecondes ou valeurs decimales
(1.7m)
Core Size I
Dimensions de Ia
carotte
Page
Collar Elevation I
Elevation du collier
Surface
Datum:
Zone:
D NAD27
D 1s D 16
r8J
[8J
17
NAD 83
D 18
Northing I Ordonnee: 5388763
Location of Core Storage I Endroit ou Ia carotte
est stockee
Datum:
D NAD27
D NAD 83
Latitude:
Longitude:
Easting I Abscisse: 4543 76
(aaaalmmljj)
Rock type I
type de roche
20 I I /05/23
Timmins- Tschupruk Road
Description (Colour, grain size, texture, minerals, alteration, etc.) I
Description (Couleur, granulometrie, texture, mineraux, transformation, etc.)
To/A
Planar Feature
Angle* I
Angle des
caracteristiques
planes
Core Specimen
Footage I
Longueur en
pieds des
carottes
pre levees
Your Sample
No./
N" d'e hantillon
du prospecteur
Sample Footage I
Niveau de
prelevement de
l'echantillon (en
pieds)
From/De
Sample
Length I
Longueur de
l'echantillon
Assays I
Analyses
mineralurgiques
To/A
Original depth of 186.0m was extended in 20 I 0 to 246.0m. This log describes
the 20 I I extension that ends at 306.0m
(246.0)
306.0
Mafic Intrusive
GABBRO
-continuation of unit that started at 213.35m.
Medium to coarse-grained groundmass- very uniform overall. Dark green
colour. again wry uniform shading in general. Massively textured throughout
except t(Jr occasional structural scams bordered by very
\\Cak
structural fabric.
Nonmagnetic throughout-- possibly weak locally. Unmineralized groundmass.
Some question as to whcthcr or not the se4ucnces is
d
massive matic flow
scqucnCL'. Homogeneity ~uggests intrusive. grain size is Sll!llewhat fine for a
*For features such as foliation. bedding. schistosity, measured from the long axis of the core.
I 'Exemples de caracteristiques :foliation. schistosite. stratification. L'angle est mesure par rapport
a I' axe longitudinal de Ia carotte.
"Mining Lands Website: http://www.mndm.gov.on.ca/mndm/mines/lands/default_e.asp"
"Stte Web de Ia Sectton des terratns mtnters: http://www.mndm.gov.on.ca/rnndmJmmes/lands/default_f.asp'
0204 (01 /2006)
© Queen·s Printer tor Ontario, 2006
~
/'7r·"~
I
© lmprimeur de Ia Reine pour !'Ontario. 2006
r')h
f >
vr
Ontario
Ministere du
Developpement du Nord
et des Mines
Drill Log
Journal de forage
Footage/Avancement
From/De
Ministry of
Northern Development
and Mines
To/A
Rock type I
type de roche
Description (Colour, grain size, texture, minerals, alteration, etc.) I
Description (Couleur, granulometrie, texture, mineraux, transformation, etc.)
EL25-08XX (second extension) cont'd
Planar Feature
Angle • I
Angle des
caracteristiques
planes
Your Sample
No.I
W d'e hantillon
du prospecteur
Core Specimen
Footage I
Longueur en
pieds des
carottes
pre levees
I
Sample Footage I
Niveau de
prelevement de
l'echantillon (en
pieds)
From/De
Page
2
Sample
Length I
Longueur de
l'echantillon
of/ de
3
Assays I
Analyses
mineralurgiques
To/A
typical gabbroic intrusion; but this may be a hypabyssal type of tiner texture.
(246.0)-251.1: texture is of coarser variety -distinctly so where crystals of .5 to
1.5 or 2mm exist. Transition is gradational over 5-l Ocm.
Homogeneity is broken only by occasional. scattered pale, whitish, mm-scale
carbonate-quartz seams of planar form- estimate I% concentration.
At 251.1 there is a gradational transition into a liner appearing phase of the
"intrusive''.
251.1-266.8: A finer looking texture but in places a coarse, faint mottle is exhibited. A fresh surface displays a finely textured, blackish groundmass.
The unit remains very homogeneous to 265.1m with occasional pale carbonatequartz seams breaking up the uniformity.
At 265.1 there is a gradational transition into a slightly pale coloured. liner
textured section of'·intrusive''. This may represent the contact phase of the
major unit that then continues trom 266.8m. Distinct contacts however are di fficult to establish. The 265.1-266.8 interval is very homogeneous and should likely
be placed as the contact zone for the next unit.
266.8-284.1: A major. uniftmn section of"gabbroic'' intrusive. Re,embles
(246.0 )-251.1 interval. Distinct crystalline groundmass of medium grain size.
Extremely homogeneous, few carbonate-quartz seams.N
Nonmagnetic.
270.4-270.5: pyritic (5~'o) white quartz-carbonate veinlet at 30 degrees to core
axis~- very sharp, planar contacts with no contact alteration effects. Sheet-like
internal structure to vein let. Pyrite occurs
in locally clotted masses.
a Ctlarsc subhedral to cuhedral crystals
II
I
·For features such as foliation. bedding, schistosity. measured from the long axis of the core. I •Exemples de caracteristiques :foliation, schistosite, stratification. L'angle est mesure par rapport
a I' axe longitudinal de Ia carotte.
"Mining Lands Website: http://www.mndm.gov.on.ca/mndm/mines/lands/default_e asp"
··site Web de Ia Section des terrains miniers : http://www mndm.gov.on.caimndm/minesllands/default_f.asp"
0204 (0 1/2006)
@Queen's Printer tor Ontario. 2006
© lmprimeur de Ia Reine pour !'Ontario, 2006
('~
t?ontario
Footage/Avancement
From/De
To!A
Ministry of
Northern Development
and Mines
Ministere du
Developpement du Nord
et des Mines
Drill Log
I Page 3
Jou rna I de forage
Rock type I
type de roche
Description (Colour, grain size, texture, minerals, alteration, etc.) I
Description (Couleur, granulometrie, texture, mineraux, transformation, etc.)
EL25-08XX (second extension) cont'd
Planar Feature
Angle* I
Angle des
caracteristiques
planes
Core Specimen
Footage I
Longueur en
pieds des
carottes
pre levees
Your Sample
No.I
N" d'e hantillon
du prospecteur
Sample Footage I
Niveau de
prelevement de
l'echantillon (en
pieds)
From/De
Sample
Length I
Longueur de
l'echantillon
of I de
3
Assays I
Analyses
mineralurgiques
To/A
278.7-278.84: Sharply defined. white quam-carbonate vein let similar to 270.4
but without pyrite. Planar 35 degree contacts. No contact alteration effects on
host '·gabbro··.
Cored surfaced ofthis phase exhibits an 8-10% presence of dark green. 1-3mm
mineral blebs disseminated through the groundmass.
At 284.1 there is a sharp contact partially preserved at 45 degrees to core axis.
284.1-285.8: Distinct, sharply defined line-grained mafic phase. Homogenous
aspect. Slight suggestion of liner texture towards contacts.
Some core breakage at both contacts - especially the upper contact.
Similar composition to enveloping mafics.
Lower contact distinct at 50 degrees to core axis. 15% white carbonate-quartz
wi~inthecon~ctover4cm.
285.8-309.0: Similar to 266.8-284.1. Medium grain size to homogenous
groundmass. Massive texture. Nonmagnetic. Unmineralized.
Homogeneity broken only by 1-2% carbonate-quartz seams and scattered, darker
green segments found to be intrinsic to the '·gabbroic'· sequence.
A very uniform section as seen in previous such sections.
306.0
[nd of Hole
*For features such as foliation. bedding. schistosity, measured from the long axis of the core.
I *Exemples de caracteristiques : foliation, schistosite, stratification. L'angle est mesure par rapport
a I' axe longitudinal de Ia carotte.
"Mining Lands Website: htip//wvw;.mndm.gov.on.ca/rnndm/mines/lands/default_e.asp"
"Site Web de Ia Section des terrains miniers : http:i/'v'rvvw.mndm.gov.on.ca/mndrn!mines/lands/default_f.asp''
0204 !01i2006)
© Queen·s Printer for Ontario, 2006
© lmprimeur de Ia Reine pour !'Ontario. 2006