NI 43-101 Technical Report for the Brewery Creek Project in North America dated October 2012 (Q29659): Difference between revisions

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data size: 10,136,863
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Revision as of 22:49, 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 Brewery Creek Project in North America dated October 2012
an NI 43-101 Technical Report pulled from the GeoArchive collection

    Statements

    addresses subject
    Cambrian Period
    concept highlight
    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
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620e687ead0e9c819b0c3456&term=Cambrian%20Period,Cambrian&dictid_filter=71&full_results&clean
    Devonian Period
    concept highlight
    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
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620e687ead0e9c819b0c3456&term=Devonian%20Period,Devonian&dictid_filter=71&full_results&clean
    Ordovician Period
    concept highlight
    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
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620e687ead0e9c819b0c3456&term=Ordovician%20Period,Ordovician&dictid_filter=71&full_results&clean
    Silurian Period
    concept highlight
    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,
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620e687ead0e9c819b0c3456&term=Silurian%20Period,Silurian&dictid_filter=71&full_results&clean
    Cretaceous Period
    concept highlight
    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
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620e687ead0e9c819b0c3456&term=Cretaceous%20Period,Cretaceous&dictid_filter=71&full_results&clean
    Jurassic Period
    concept highlight
    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
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620e687ead0e9c819b0c3456&term=Jurassic%20Period,Jurassic&dictid_filter=71&full_results&clean
    metadata URL
    https://w3id.org/usgs/z/4530692/K2MVUCBK
    MIME type
    text/html
    application/json
    0 references
    P142 (Deleted Property)
    77,017 Property P142 not found, cannot determine the data type to use.
    0 references
    P143 (Deleted Property)
    4B6BZBPR Property P143 not found, cannot determine the data type to use.
    data size
    10,136,863
    0 references
     
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