NI 43-101 Technical Report for the Shorty Creek Project in Alaska, United States dated March 2015 (Q28661)
From geokb
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 Shorty Creek Project in Alaska, United States dated March 2015 |
an NI 43-101 Technical Report pulled from the GeoArchive collection |
Statements
lithologies can be pervasively altered and mineralized. Devonian volcanic rocks and Cretaceous dikes represent
complex and poorly understood belt of Paleozoic through Cretaceous sedimentary, metamorphic and intrusive
the Wilber Creek unit, a folded sequence of Early Cretaceous flysch sediments which form the youngest
felsic dikes and sills that intrude the Jurassic-Cretaceous Wilber Creek flysch sequence. Data from
(Weber and others, 1992; Weber and others, 1997). Late Cretaceous and Tertiary dextral motion along the
Tintina fault in the Yukon Territory. During Mid-Cretaceous time, the Livengood area was 27
Livengood Terrane have been intruded by both mid-Cretaceous (90 to 110 Ma) and Early Tertiary (60-75
conglomerate unit suggest a Late Jurassic to Early Cretaceous age although Weber and others (1997)
others (1997) assign the Wilber Creek rocks an Early Cretaceous age in the Shorty Creek project area. The
occurrences which appear to be genetically related to mid-Cretaceous (90-110 Ma) and early Tertiary (60-75
altered and mineralized. Devonian volcanic rocks and Cretaceous dikes represent the most favorable host
M.L., 1997, Precious metals associated with Late Cretaceous – early Tertiary igneous complexes of
Hart, C., 2000, Exploration models for mid and Late Cretaceous intrusion-related gold deposits in Alaska
Mair, John L., 2004, The northern cordilleran mid-Cretaceous plutonic province: ilmenite/magnetite-series
Heffernan, S., 2000, Temporal evolution of early and mid-Cretaceous magmatism in the Tintina Gold Belt: The
with the felsic dikes and sills that intrude the Jurassic-Cretaceous Wilber Creek flysch sequence.
pelecypods within the conglomerate unit suggest a Late Jurassic to Early Cretaceous age although Weber
by 600 meters. Mineralization remains open under Quaternary cover on both ends. Mineralization at
1700 meters by 600 meters and remains open under Quaternary cover on both ends. The north and south
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:QGQNMNKK Property P97 not found, cannot determine the data type to use.
0 references
