NI 43-101 Technical Report for the Haile Project in South Carolina, United States dated April 2010 (Q31718): Difference between revisions

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Revision as of 19:21, 11 March 2024

an NI 43-101 Technical Report pulled from the GeoArchive collection
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NI 43-101 Technical Report for the Haile Project in South Carolina, United States dated April 2010
an NI 43-101 Technical Report pulled from the GeoArchive collection

    Statements

    metamorphosed sedimentary rocks of Late Proterozoic or Early Cambrian age. This volcanic arc assemblage was deposited
    present within all of the Late Proterozoic to Early Cambrian aged units. This deformation manifests
    laminated sediments of Late Precambrian or earliest Cambrian age. The mineralization was driven by hydrothermal
    metavolcaniclastic and upper metasedimentary rocks of Precambrian/Cambrian transition age (560 million years ago (Ma))
    strain is present within all of the Precambrian to Cambrian aged units. This deformation manifests
    textures of the rocks. Regional submersion during the Cretaceous resulted in the deposition of kaolinite
    metasedimentary lithologies. 7.1.1.6 Coastal Plain Sand The Cretaceous Middendorf Formation can have thicknesses
    metasediments, saprolite, Mesozoic diabase dikes, and Cretaceous coastal plain sand were updated with
    Sand A wire-mesh surface of the basal contact of the Cretaceous aged Middendorf Formation was created
    deposition of Coastal Plain sediments during the Cretaceous. The area has since gone through continental
    laminated metasiltstone. 7.1.4.6 Coastal Plain Sand The Cretaceous Middendorf Formation can have thicknesses
    units are crosscut by northwesttrending, Triassic to Jurassic age diabase dikes. Saprolite of variable
    assemblage is crosscut by northwest-trending, Triassic to Jurassic age diabase dikes. Saprolite of variable
    while areas of metasedimentary rocks are unpatterned (Triassic rift basins not shown). Generalized slate
    sheared. These units are crosscut by northwesttrending, Triassic to Jurassic age diabase dikes. Saprolite
    entire assemblage is crosscut by northwest-trending, Triassic to Jurassic age diabase dikes. Saprolite
    2 references
    Linkage to this mine was established with a simple name match from imperfect metadata identifying the geographic area of the mining project
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    77,058
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    X499PF9S
    application/pdf
    3804d8d3733a1db74ad9f97477a2b94a
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