The Ware map area, containing 31 documented mineral occurrences, is divided
by the Rocky Mountain Trench into two geologically distinct regions.
Bulletin 103: Geology of the
Aikie River Area Northeast British Columbia (NTS 94F), by D.G. MacIntyre.
The Autodesk WHIP!® viewer is
required to view this map.
Southwest of the trench, clastics and carbonates (and metamorphic equivalents)
of the Proterozoic Ingenika Group are locally intruded by Tertiary granites and quartz
monzonites. This area hosts the Fox
Pass (094F 006) tungsten-copper-molybdenum showing.
Northeast of the trench, thick packages of mid-Proterozoic to mid-Paleozoic
basinal sediments and platformal carbonates were deposited along the Ancestral North
America terrane continental shelf. Periodic rifting and tectonic subsidence resulted in
the formation of starved sub-basins along this otherwise passive continental margin. One
of these sub-basins, the Kechika trough, hosts sedimentary exhalative barite and
barite-sulphide deposits in sediments of Middle Ordovician, Early Silurian, and Late
Devonian age. The latter are the most significant type and are hosted by carbonaceous
cherty argillites and siliceous shales of the Upper Devonian Gunsteel Formation of the
Devonian to Mississippian Earn Group. Curragh Resources' Cirque
(Stronsay) (094F 008) deposit, boasting reserves in excess of 35 million tonnes,
averaging 10 per cent combined lead-zinc and 47.5 grams per tonne silver, is planned for
development with mine construction possibly commencing in the summer of 1992. Other
similar deposits that are potentially significant in the map area include Fluke,
Elf,
Mt.
Alcock, Pie,
and Bear,
(094F 009, 011, 015, 023, and 024, respectively).
In the northeast corner of the map sheet, copper replacement deposits, such as
the Blue,
Grayling,
Waterfall,
Atan
Copper and Grayling
Creek showings (094F 005, 012, 014, 028, and 029, respectively), occur within
Lower Cambrian to Silurian platform carbonates.
In the central portion of the map area, the Fram
(094F 004) copper vein deposits are hosted within Helikian to Lower Cambrian
carbonates exposed in the Muskwa anticlinoria.

REFERENCES
Aeromagnetic Colour Maps (1999): Aeromagnetic Residual Total Field of 094E
and F, Geological Survey of Canada, Open File 3495, 1:100,000-scale, 8 sheets.
MacIntyre, D.G. (1998): Geology of the Aikie River Area Northeast British
Columbia (NTS 94F), B.C. Ministry of Energy and Mines, Bulletin 103, scale 1:100,000. The Autodesk WHIP!® viewer is required to
view this map.
Gabrielse, H. (1977): Geological Map of Ware (094F west half) and Toodoggone
River (094E) map areas; Geological Survey of Canada, Open File 483, scale
1:125,000.
Taylor, G.C., compiler (1979): Geological Map of the Ware (094F east half) and
Trutch (094G) map areas; Geological Survey of Canada, Open File 606, scale
1:125,000.
BC Geological Survey Publications for NTS 094F
