NI 43-101 Technical Report for the Yauricocha Project in Peru dated October 2019 (Q32259): Difference between revisions
From geokb
(Created a new Item: Added initial NI 43-101 item from Zotero library) |
(Cleared an Item: Added claims for geochronologic period based on xDD snippet extraction) |
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| Property / addresses subject | |||
| Property / addresses subject: Cretaceous Period / rank | |||
Normal rank | |||
| Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: Marianatype subduction from the Late Triassic to Late Cretaceous and Andean-style subduction from the | |||
| Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: Cretaceous and Andean-style subduction from the Late Cretaceous to the present. Late Triassic to late | |||
| Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: Cretaceous to the present. Late Triassic to late Cretaceous Mariana-type subduction resulted in an | |||
| Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: Formation The oldest rocks exposed in the area are the lower Cretaceous Goyllarisquizga arenites. This formation | |||
| Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: outcrops in the Éxito zone. Jumasha Formation The mid-Cretaceous Jumasha Formation consists of massive | |||
| Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: contact. It has been assigned an age between upper Cretaceous and lower Tertiary, but because of the | |||
| Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: The stock intrudes tightly folded beds of the late Cretaceous Jumasha and Celendín Formations and the | |||
| Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: Formations and the overlying Casapalca Formation (latest Cretaceous and Paleocene?). Mineralized bodies are | |||
| Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: tests from 10 drill holes] Casapalca Formation (late Cretaceous to Tertiary): interbedded silty limestone, | |||
| Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: from 9 drill holes] The Celendin Formation (Late Cretaceous) Celendin Formation is made principally | |||
| Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: 4 drill holes] Jumasha Formation (Middle to Late Cretaceous) The Jumasha Formation is comprised | |||
| Property / addresses subject: Cretaceous Period / reference | |||
| Property / addresses subject: Cretaceous Period / reference | |||
| Property / addresses subject | |||
| Property / addresses subject: Triassic Period / rank | |||
Normal rank | |||
| Property / addresses subject: Triassic Period / qualifier | |||
concept highlight: volcanism to Upper Paleozoic time. Beginning in the Late Triassic time, following Atlantic Ocean rifting, | |||
| Property / addresses subject: Triassic Period / qualifier | |||
concept highlight: present Andes: the Marianatype subduction from the Late Triassic to Late Cretaceous and Andean-style subduction | |||
| Property / addresses subject: Triassic Period / qualifier | |||
concept highlight: subduction from the Late Cretaceous to the present. Late Triassic to late Cretaceous Mariana-type subduction | |||
| Property / addresses subject: Triassic Period / reference | |||
| Property / addresses subject: Triassic Period / reference | |||
| Property / addresses subject | |||
| Property / addresses subject: Quaternary Period / rank | |||
Normal rank | |||
| Property / addresses subject: Quaternary Period / qualifier | |||
concept highlight: Hydrostratigraphic units are defined based on geology: Quaternary Sediments: colluvium, moraine and alluvial | |||
| Property / addresses subject: Quaternary Period / qualifier | |||
concept highlight: metallurgical mining activities; • Air quality - Bi-quaternary monitoring is performed in two monitoring | |||
| Property / addresses subject: Quaternary Period / qualifier | |||
concept highlight: monitoring results are yet available; • Noise: Bi-quaternary monitoring is performed in three monitoring | |||
| Property / addresses subject: Quaternary Period / qualifier | |||
concept highlight: Decree N° 085-2003-PCM; • Soil quality monitoring - Quaternary monitoring is performed in three monitoring | |||
| Property / addresses subject: Quaternary Period / qualifier | |||
concept highlight: piezometers. • Emissions and dust control: – Bi-quaternary monitoring two monitoring stations: one | |||
| Property / addresses subject: Quaternary Period / qualifier | |||
concept highlight: established monitoring frequency for the first two years is quaternary, and for the following three years biannual. | |||
| Property / addresses subject: Quaternary Period / reference | |||
| Property / addresses subject: Quaternary Period / reference | |||
Revision as of 20:51, 19 April 2023
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
