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 20:25, 11 March 2024
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 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;
76,998
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