NI 43-101 Technical Report for the Macktush Project in North America dated July 2015 (Q30687)
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 Macktush Project in North America dated July 2015 |
an NI 43-101 Technical Report pulled from the GeoArchive collection |
Statements
Group, or sandstones, shales and conglomerates of the Cretaceous Nanaimo Group. The Macktush property
Triassic and Jurassic), one major sedimentary event (Cretaceous) and four major intrusive events (Triassic,
Group, sandstones, shales and conglomerates of the Cretaceous Nanaimo Group. All units are occasionally
granodiorite sills, stocks -6- and dikes of the Jurassic Island plutonic suite. Local inliers consist
sedimentary limestones of the Vancouver Group overlain by Jurassic sediments and volcanics of the Bonanza
volcano-sedimentary events (Paleozoic, Triassic and Jurassic), one major sedimentary event (Cretaceous)
(Cretaceous) and four major intrusive events (Triassic, Jurassic, Eocene and Miocene/Pliocene). Major structural
large granodiorite sills, stocks and dikes of the Jurassic Island plutonic suite. Locally inliers
limestones of the Vancouver Group that are overlain by Jurassic volcanics of the Bonanza Group, sandstones,
of the David Vein is sheared granodiorite of the Jurassic island plutonic suite, which occasionally
sheared granodiorite or quartz feldspar porphyry of the Jurassic island plutonic suite. The only available
sheared granodiorite or quartz feldspar porphyry of the Jurassic island plutonic suite. It is currently
rock of the Moly Vein is sheared granodiorite of the Jurassic island plutonic suite, which occasionally
thick) feldspar porphyry dikes and/or sills of the Jurassic Island plutonic suite, which occur mainly
and the overlying Triassic Quatsino Limestone, and Jurassic Island Intrusive stocks, dikes and sills,
flank of a volcano-sedimentary basin underlain by Jurassic Bonanza volcanics and immediately north
hornfelsed metamorphic aureole of the NNW-trending Jurassic intrusive big dike which transects the
stratigraphic horizon as Target A, along the base of the Jurassic Bonanza volcanics immediately above the
close to and possibly intruded by a large body of Jurassic age Island Suite granodioritic intrusives
Quatsino Formation limestones unconformably overlain by Jurassic Bonanza Group volcanics and volcaniclastics.
immediate Port Alberni area is mainly underlain by Triassic mafic volcanic rocks of the Karmutsen Formation
Jurassic Island plutonic suite. Local inliers consist of Triassic Quatsino Formation sedimentary limestones
three major volcano-sedimentary events (Paleozoic, Triassic and Jurassic), one major sedimentary event
event (Cretaceous) and four major intrusive events (Triassic, Jurassic, Eocene and Miocene/Pliocene).
Falls Uplift to the northwest. Small stocks of the Triassic Mount Hall Gabbro suite occasionally intrude
Island plutonic suite. Locally inliers consist of Triassic Quatsino Formation sedimentary limestones
occasionally contains altered xenoliths of presumably Triassic Karmutsen volcanics or Paleozoic Buttle
occasionally contains altered xenoliths of presumably Triassic Karmutsen volcanics. It was exposed and
Dauntless North Veins are brecciated to pillowed Triassic Karmutsen mafic volcanics, with occasional
rock consists of pillowed mafic volcanics of the Triassic Karmutsen Formation with minor quartz-feldspar
in turn intrudes brecciated mafic volcanics of the Triassic Karmutsen Formation. Sub-parallel, more
contact of the Karmutsen volcanics and the overlying Triassic Quatsino Limestone, and Jurassic Island
092F412 sedimentary limestone showing, hosted in the Triassic Quatsino Limestone. Quartz diorite on the
Jurassic Bonanza volcanics and immediately north and the Triassic Quatsino limestones. Mapping also indicates
Jurassic Bonanza volcanics immediately above the Triassic Quatsino limestones. It also lies along
basin. This portion of the basin conformably overlies Triassic age Karmutsen Formation mafic volcanics,
dikes of unknown age. The basin itself consists of Triassic Quatsino Formation limestones unconformably
P142 (Deleted Property)
77,038 Property P142 not found, cannot determine the data type to use.
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