NI 43-101 Technical Report for the Brewery Creek Project in North America dated October 2012 (Q29659)
From geokb
an NI 43-101 Technical Report pulled from the GeoArchive collection
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | NI 43-101 Technical Report for the Brewery Creek Project in North America dated October 2012 |
an NI 43-101 Technical Report pulled from the GeoArchive collection |
Statements
Property are composed of Rabbitkettle Formation (Cambrian-Ordovician) calcareous phyllite overlain
Volcanics, Diment and Craig (1999) suggest a late Cambrian to early Ordovician age. 7.2.1.3 Road River
unit extended from the Devonian through the early Carboniferous. It is likely that the Earn group
property. During the Proterozoic and again in the late Devonian, the basin was subjected to rifting accompanied
sediments. During the Proterozoic and again in the late Devonian, the basin was subjected to rifting. This
volcanics and off-shelf sediments and Earn Group (Lower Devonian) shelf siliciclastics. Throughout most
placed thin sequences of Silurian siltstones against Devonian siliciclastics. The age of thrusting is
Formation have been identified as Silurian to early Devonian in age (Norford and Poulton, 1995). The
suggests that deposition of this unit extended from the Devonian through the early Carboniferous. It is
Suite felsic rocks intruding through Ordovician to Devonian aged marine off-shelf and platform sedimentary
are composed of Rabbitkettle Formation (Cambrian-Ordovician) calcareous phyllite overlain by Road
calcareous phyllite overlain by Road River Group (Ordovician-Silurian) volcanics and off-shelf sediments
property, it has been interpreted as old as Cambro-Ordovician 24 BREWERY CREEK NI 43-101 TECHNICAL
1981; Thompson et al., 1992) and as young as mid-Ordovician (Gordey and Anderson, 1993). The Rabbitkettle
and Craig (1999) suggest a late Cambrian to early Ordovician age. 7.2.1.3 Road River Group This stratigraphic
aged Tombstone Suite felsic rocks intruding through Ordovician to Devonian aged marine off-shelf and
phyllite overlain by Road River Group (Ordovician-Silurian) volcanics and off-shelf sediments and
thrust faulting that has placed thin sequences of Silurian siltstones against Devonian siliciclastics.
assemblages in the Steel Formation have been identified as Silurian to early Devonian in age (Norford and Poulton,
Reserve Trend. The sills were emplaced as part of the Cretaceous Tombstone Suite and typically were emplaced
siliciclastics. Throughout most of the Property, Cretaceous monzonite and quartz monzonite intrudes
semi-conformable sills along a 15 kilometres strike length. Cretaceous (91 Ma), Tombstone Suite biotite monzonite
of thrusting is probably related to the earliest Cretaceous movement on the Tombstone Thrust. A property
mineralization at Brewery Creek is hosted within mid-Cretaceous, felsic intrusive rocks of the Tombstone
is related to late ore forming fluids derived from Cretaceous aged Tombstone Suite felsic rocks intruding
emplacement of thick sills of intrusive rocks. By late Jurassic, the rocks of the Intermontane Belt of
shows that thrust faulting took place between late Jurassic and midCretaceous time based on the age
Strain Zone, a cross cutting structural feature. The Jurassic date is consistent with thrust faults mapped
southwest. The Tintina Fault, is interpreted as a Paleogene-aged dextral strike-slip fault with an
P142 (Deleted Property)
77,017 Property P142 not found, cannot determine the data type to use.
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