FOR MORE INFORMATION CONTACT: Jeff Ledrew

Transcription

FOR MORE INFORMATION CONTACT: Jeff Ledrew
NEWFOUNDLAND & LABRADOR
Explore The Opportunities
Brigus Au-Cu
FR
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NT
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PP
LA
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100km
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CENTRAL (IAPETAN)
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HU
MB
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MOBILE BELT
MIOGEOCLINAL
COVER
3.6 g/t Au
2.31% Cu,
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15 ppb Au
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BRIGUS
PROPERTY
Map 1. Property Location Map
Local Geology
The Drook Formation (Conception Group) underlies the western side of the property and comprises green siliceous siltstone
and sandstone and silicified tuff. The Brigus Fault (Map 2) separates the latter unit from the Harbour Main Group in the centre
of the property, comprising pink to grey felsic tuff and agglomerate, rhyolite and welded tuff and locally amygdaloidal basalt
flows, interbedded with basalt breccia and sedimentary rocks. The Brigus Fault is associated with hydrothermal
alteration and gold mineralization elsewhere in the Avalon Zone (O’Brien and O’Driscoll, 1996). The Conception
Group is brecciated along the fault.
Drook Fm - Siliciclastics
Brigus Lookout Au Showing
Vocanic rocks showing extensive hematization
Mineralized Quartz Vein
Mineralization
Murray (1880) investigated the reported presence of gold in quartz veins occurring throughout the Brigus area. Grab
samples taken in the early 1990’s returned up to 0.71% Cu (McNamara, 1991). Prospecting in the mid to late 1990’s
(Snow, 2001) resulted in anomalous gold values obtained on several parts of the property, both in quartz veins and
hydrothermally altered rhyolite and basalt flows and breccias. Gold values up to 464 ppb were returned for grab
samples of quartz veins in basalt taken near Brigus Lookout (Brigus Lookout Au Showing, Map 2). These quartz
veins are up to 40 cms across, contain disseminated pyrite, chalcopyrite and bornite, chlorite and in some localities,
abundant epidote. Blocks of wall rock are locally incorporated in the veins. One vein trending N-S runs anomalous
gold consistently (150 to 454 ppb) and can be traced for more than 0.5 km. Basalts locally contain chalcocite and
malachite, with no development of quartz veins, and in places are in contact with rusty, silicified rhyolite and breccia.
Altered mafic volcanic and mafic intrusive rock near Brigus Lookout assayed 284 ppb Au. Cu values > 2200 ppm
associated with elevated gold (53 ppb) occur in altered rhyolite with malachite staining.
The present owner has resampled the main quartz vein in several places. The best grab taken from the northern
exposure of the vein (Map 2) returned 3.614 g/t Au and 2.31% Cu. The best grab taken from a southern exposure of
the vein on the property returned 0.76% Cu and 45 g/t Ag. Some of the quartz in this vein is chalcedonic and in
places shows a fine banding defined by alternating light and dark grey layers.
Mineralization Model
Produced By:
Detailed mapping needs to be carried out on the property in order to be able to define possible deposit types and to assess the
spatial relations of the Brigus Fault to any
mineralization. Much of the area has extensive
FOR MORE INFORMATION CONTACT: bush
prospectors
cover and requires an extensive soil grid resource
room
Jeff Ledrew
to properly evaluate blind mineralization.
However, mineralization has been found in October, 2012
Telephone: (709)-727-8850
both the basalt and rhyolite host rocks and may
E-mail: jeff_ledrew@hotmail.com
be of the Volcanic-associated Redbed Copper type.
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0.756% Cu, 45 g/t Ag
Harb
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Fels ur Main
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Brig us Faul t
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Regional Geology
The property lies within the Avalon Tectonostratigraphic Zone of the Newfoundland Appalachians and is underlain by two
principal rock units - the Harbour Main and Conception groups. The Proterozoic Harbour Main Group is a sequence of
volcanic and associated sedimentary rocks and the late Neoproterozoic Conception Group comprises turbidites.
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Bri g
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Si lic s F m
iclas
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The Brigus Property consists of 15 claims located on Brigus Head, 1 km east of Cupids on the Avalon Peninsula of
Newfoundland and Labrador, (NTS 1N/11). The property is easily accessed on foot from trails in Cupids.
ISLAND OF
NEWFOUNDLAND
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Soil Samples
Rock Samples
Historical Gold Occurrence
Map 2. Property Claims Location and Geology Map
Source: King, A.F.: Geology of the Avalon Peninsula,
Newfoundland (parts of 1K, 1L,1M,1N and 2C). Newfoundland
Department of Mines, Mineral Development Division, Map 88-01.