NI 43-101 Technical Report for the Yauricocha Project in Peru dated October 2019 (Q32259)

From geokb
Revision as of 20:51, 19 April 2023 by Sky (talk | contribs) (‎Cleared an Item: Added claims for geochronologic period based on xDD snippet extraction)
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 Yauricocha Project in Peru dated October 2019
an NI 43-101 Technical Report pulled from the GeoArchive collection

    Statements

    Marianatype subduction from the Late Triassic to Late Cretaceous and Andean-style subduction from the
    Cretaceous and Andean-style subduction from the Late Cretaceous to the present. Late Triassic to late
    Cretaceous to the present. Late Triassic to late Cretaceous Mariana-type subduction resulted in an
    Formation The oldest rocks exposed in the area are the lower Cretaceous Goyllarisquizga arenites. This formation
    outcrops in the Éxito zone. Jumasha Formation The mid-Cretaceous Jumasha Formation consists of massive
    contact. It has been assigned an age between upper Cretaceous and lower Tertiary, but because of the
    The stock intrudes tightly folded beds of the late Cretaceous Jumasha and Celendín Formations and the
    Formations and the overlying Casapalca Formation (latest Cretaceous and Paleocene?). Mineralized bodies are
    tests from 10 drill holes] Casapalca Formation (late Cretaceous to Tertiary): interbedded silty limestone,
    from 9 drill holes] The Celendin Formation (Late Cretaceous) Celendin Formation is made principally
    4 drill holes] Jumasha Formation (Middle to Late Cretaceous) The Jumasha Formation is comprised
    volcanism to Upper Paleozoic time. Beginning in the Late Triassic time, following Atlantic Ocean rifting,
    present Andes: the Marianatype subduction from the Late Triassic to Late Cretaceous and Andean-style subduction
    subduction from the Late Cretaceous to the present. Late Triassic to late Cretaceous Mariana-type subduction
    Hydrostratigraphic units are defined based on geology: Quaternary Sediments: colluvium, moraine and alluvial
    metallurgical mining activities; • Air quality - Bi-quaternary monitoring is performed in two monitoring
    monitoring results are yet available; • Noise: Bi-quaternary monitoring is performed in three monitoring
    Decree N° 085-2003-PCM; • Soil quality monitoring - Quaternary monitoring is performed in three monitoring
    piezometers. • Emissions and dust control: – Bi-quaternary monitoring two monitoring stations: one
    established monitoring frequency for the first two years is quaternary, and for the following three years biannual.
    2 references
    Linkage to this mine was established with a simple name match from imperfect metadata identifying the geographic area of the mining project
    P97 (Deleted Property)
    4530692:8IDS7IMI Property P97 not found, cannot determine the data type to use.
    0 references