(Q34681)
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:
text/html
application/json
0 references
application/vnd.apache.parquet
1d7b4ebc7390a90efb7f0ad84cf82808839f763898feefc37a628432b416b05d
a4744e4d5b06c8b47f8ae3fcbcfcaec7
141,883
0 references
application/pdf
118d30f5402416c3bc0926253f27b51ba835f1ca09d082ca9ce20e1125c6c586
5bb606b97ae7b248fc071ddc3663f09f
19,003,731
0 references