NI 43-101 Technical Report for the Macktush Project in North America dated July 2015 (Q30687): Difference between revisions

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Revision as of 23:05, 29 August 2023

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

    addresses subject
    Cretaceous Period
    concept highlight
    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
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620cf224ad0e9c819b050db6&term=Cretaceous%20Period,Cretaceous&dictid_filter=71&full_results&clean
    Jurassic Period
    concept highlight
    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.
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620cf224ad0e9c819b050db6&term=Jurassic%20Period,Jurassic&dictid_filter=71&full_results&clean
    Triassic Period
    concept highlight
    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
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620cf224ad0e9c819b050db6&term=Triassic%20Period,Triassic&dictid_filter=71&full_results&clean
    metadata URL
    https://w3id.org/usgs/z/4530692/NN8EK7UJ
    MIME type
    text/html
    application/json
    0 references
    P142 (Deleted Property)
    77,038 Property P142 not found, cannot determine the data type to use.
    0 references
    P143 (Deleted Property)
    P6W6U9CE Property P143 not found, cannot determine the data type to use.
    data size
    19,495,371
    0 references
     
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