67755 093N 154 093N6 Cu4 Omineca LO 093N045 093N06E Showing 55° 25' 30'' 125° 09' 06'' 55.425000 -125.151667 10 6143974 363932 Copper Intermontane Plutonic Rocks L03 : Alkalic porphyry Cu-Au The Lo occurrence is situated in the Kwanika Range near the headwaters of Halobia Creek, approximately 51 kilometres east-southeast of Takla Landing. The area was the subject of a program of soil geochemistry undertaken by Noranda Exploration in 1972. The Halobia Creek area is underlain by mesozonal plutonic rocks assigned to the Late Triassic to Early Cretaceous Hogem Intrusive Complex which have intruded volcanic and sedimentary rocks of the Middle Triassic to Lower Jurassic Takla Group east of the Pinchi fault zone. The plutonic rocks form an elongate batholith, extending from Chuchi Lake, north to the Mesilinka River. The only reference to the Lo occurrence describes chalcopyrite mineralized fractures and disseminations in syenodiorite (Geology, Exploration and Mining in British Columbia 1972, page 448). No recent information concerning this occurrence is available. EMPR GEM *1972-448 EMPR BULL 70 EMPR PF (Peto, P. (1971): Report on the Hogem Project for Amoco Mining (refer to 093N General File)) GSC MEM 252 GSC MAP 844A; 907A; 971A; 1424A GSC P 42-7; 45-6 GSC OF 3071 CIM Vol. 67, No. 749, pp. 101-106 EMPR PFD 860499, 862384, 862386, 671090, 671091, 671092, 671093, 671094, 671095, 671096, 672142, 672143, 672144, 672454, 673478, 673479, 674040, 674557