NI 43-101 Technical Report for the Kena Project in North America dated May 2013 (Q34681): Difference between revisions

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Latest revision as of 15:14, 19 November 2024

an NI 43-101 Technical Report pulled from the GeoArchive collection
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NI 43-101 Technical Report for the Kena Project in North America dated May 2013
an NI 43-101 Technical Report pulled from the GeoArchive collection

    Statements

    addresses subject
    Jurassic Period
    concept highlight
    MINERALIZATION The Kena property lies within lower-Jurassic Elise Formation (Fm) mafic volcanics and
    sediments that were accreted to North America in Middle Jurassic time. These rocks tectonically overlie
    PROPERTY GEOLOGY Kena mineralization occurs within lower Jurassic Elise Fm (Rossland Gp) mafic volcanics
    (Rossland Gp) mafic volcanics and associated mid-Jurassic Silver King intrusive rocks (Figure 3). 7.2.1
    is documented in BCGS Bulletin 102, titled “Early Jurassic Rossland Group, Southern British Columbia
    potassium or alkaline character of many synvolcanic Early Jurassic plutons. 7.2.2 AREAS OF INTEREST AND MINERALIZATION Gold
    Paper 1989-1. HOY, T. and DUNNE, K.P.E., 1997; Early Jurassic Rossland Group – Part I Stratigraphy and
    DANDY, L.L., 2003; Gold Mountain Zone – Early-Middle Jurassic Porphyry Au+/-Cu Mineralization, SEBC:
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620cf21dad0e9c819b05064d&term=Jurassic%20Period,Jurassic&dictid_filter=71&full_results&clean
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