NI 43-101 Technical Report for the Nieves Project in North America dated August 2012 (Q28681): Difference between revisions

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Revision as of 22:41, 29 August 2023

an NI 43-101 Technical Report pulled from the GeoArchive collection
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English
NI 43-101 Technical Report for the Nieves Project in North America dated August 2012
an NI 43-101 Technical Report pulled from the GeoArchive collection

    Statements

    between the Guerrero Terrane rocks and younger Jurassic-Cretaceous sedimentary sequences (interpreted to
    Caracol Formation on the Property) is unclear. The late Cretaceous to early Tertiary Laramide Orogeny folded
    in the western Altiplano are units from the late Cretaceous to Tertiary, Sierra Madre Occidental
    These rocks consist of a lower assemblage of late Cretaceous to Tertiary volcanic, volcaniclastic,
    been assigned to the Caracol Formation of the late Cretaceous age. Argillite beds are more abundant
    to compression during the Laramide Orogeny in the Cretaceous. Thrust faults are also common features
    the Fresnillo District are underlain by a Jurassic-Cretaceous turbidite flysch sequence (Nieves; appears
    argillic alt., domes, silicification volarenite Cretaceous Early Late Cuestra del Cerro Gordo 300 Limestone Replacement
    boundary between the Guerrero Terrane rocks and younger Jurassic-Cretaceous sedimentary sequences (interpreted
    Property and the Fresnillo District are underlain by a Jurassic-Cretaceous turbidite flysch sequence (Nieves;
    0 references
    76,998
    0 references
    T3I3S8DR
    27,576,769
    0 references