NI 43-101 Technical Report for the Kena Project in North America dated May 2013 (Q34681): Difference between revisions
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Revision as of 23:53, 17 November 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 Kena Project in North America dated May 2013 |
an NI 43-101 Technical Report pulled from the GeoArchive collection |
Statements
of accreted rocks with North America – include the Cretaceous Sophie Mountain Formation and Eocene
MINERALIZATION The Kena property lies within lower-Jurassic Elise Formation (Fm) mafic volcanics and
sediments that were accreted to North America in Middle Jurassic time. These rocks tectonically overlie
PROPERTY GEOLOGY Kena mineralization occurs within lower Jurassic Elise Fm (Rossland Gp) mafic volcanics
(Rossland Gp) mafic volcanics and associated mid-Jurassic Silver King intrusive rocks (Figure 3). 7.2.1
is documented in BCGS Bulletin 102, titled “Early Jurassic Rossland Group, Southern British Columbia
potassium or alkaline character of many synvolcanic Early Jurassic plutons. 7.2.2 AREAS OF INTEREST AND MINERALIZATION Gold
Paper 1989-1. HOY, T. and DUNNE, K.P.E., 1997; Early Jurassic Rossland Group – Part I Stratigraphy and
DANDY, L.L., 2003; Gold Mountain Zone – Early-Middle Jurassic Porphyry Au+/-Cu Mineralization, SEBC:
P143 (Deleted Property)
C4HHPV2T Property P143 not found, cannot determine the data type to use.
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