NI 43-101 Technical Report (OM) for the Reefton Project in Australasia, New Zealand dated 2013 (Q31818): Difference between revisions

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Revision as of 23:14, 29 August 2023

an NI 43-101 Technical Report pulled from the GeoArchive collection
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English
NI 43-101 Technical Report (OM) for the Reefton Project in Australasia, New Zealand dated 2013
an NI 43-101 Technical Report pulled from the GeoArchive collection

    Statements

    Alpine Fault. The Reefton Goldfield is hosted by early Ordovician age Greenland Group meta-sedimentary
    2013 TECHNICAL REPORT REEFTON PROJECT During the Late Ordovician or Early Silurian, the Greenland Group
    rocks in New Zealand. The Late Cambrian to Early Ordovician age range has been allocated on the basis
    & Craw, 1994). 6.4.3 Deformation During the late Ordovician to Early Silurian, east-west compression
    REPORT REEFTON PROJECT During the Late Ordovician or Early Silurian, the Greenland Group was subjected to lower
    1994). 6.4.3 Deformation During the late Ordovician to Early Silurian, east-west compression resulted in the
    concurrent granitoid pluton emplacement during the Silurian led to the development of a weak, pervasive,
    Devonian to Carboniferous (Tuhua Phase) and lower-mid Cretaceous (Rangitata Phase) granitoid plutons. Mafic
    of the Kirwan Intrusive were emplaced during the Cretaceous. Some of these mafic dykes occur in the
    west, the fault contact is obscured by Tertiary and Quaternary sediments which fill the Grey-Inangahua
    with significant surface rupture of a major late Quaternary active fault trace and no surface rupture
    2 references
    Linkage to this mine was established with a simple name match from imperfect metadata identifying the geographic area of the mining project
    0 references
    77,060
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    6XVQWZAN
    8,345,050
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