General Information
Deposit Type(s): Unknown
Location(s): 64°34'37" N - -138°19'6" W
NTS Mapsheet(s): 116B09
Location Comments: .5 Kilometres
Hand Samples Available: No
Last Reviewed:
Capsule
Work History
Staked as CEC cl 1-4 (YBI7452) in Jul/88 by G. Freibergs, who transferred a 67% interest to C. McLennan in Jul/89.
In Apr/97 Canadian United Minerals Inc staked Ree N-W cl 1-12 (YC03901) 7.5 km to the northwest and Ree West cl 1-12 (YC04003) 3 kms to the west and carried out prospecting and magnetometer surveying of both claim blocks in Mar/98.
Capsule Geology
The CEC claims covered a contact between volcanic and sedimentary rocks of Proterozoic or Cambrian age.
Canadian United's claims blocks are underlain by Marmot Formation amygdaloidal basalt, of Lower Cambrian to Lower Ordovician age. Magnetic response was flat over the Ree N-W claims and was flat over most of the test line on the Ree West claims, except for two moderately magnetic features of unknown source detected at the west end of the line. No mineralization was found on either claim block.
These areas now lie within the boundaries of the Tombstone Territorial Park and have been withdrawn from staking.
References
BREMNER, T.J., 1994. Proposed Tombstone Park: Preliminary Review of Mineral Potential. Exploration and Geological Services Division, Indian and Northern Affairs Canada. Open File 1994-2(T), 115 p.
CANADIAN UNITED MINERALS INC, Sep/98. Assessment Report #093930 by S. Ryan.
CANADIAN UNITED MINERALS INC, Sep/98. Assessment Report #093932 by S. Ryan.
THOMPSON, R.I., ROOTS, C.F. AND MUSTARD, P.S., 1992. Geology of Dawson map area (116B, C) (northeast of Tintina Trench); Geological Survey of Canada, Open File 2849 (13 sheets, scale: 1:50 000).
Staked as CEC cl 1-4 (YBI7452) in Jul/88 by G. Freibergs, who transferred a 67% interest to C. McLennan in Jul/89.
In Apr/97 Canadian United Minerals Inc staked Ree N-W cl 1-12 (YC03901) 7.5 km to the northwest and Ree West cl 1-12 (YC04003) 3 kms to the west and carried out prospecting and magnetometer surveying of both claim blocks in Mar/98.
Capsule Geology
The CEC claims covered a contact between volcanic and sedimentary rocks of Proterozoic or Cambrian age.
Canadian United's claims blocks are underlain by Marmot Formation amygdaloidal basalt, of Lower Cambrian to Lower Ordovician age. Magnetic response was flat over the Ree N-W claims and was flat over most of the test line on the Ree West claims, except for two moderately magnetic features of unknown source detected at the west end of the line. No mineralization was found on either claim block.
These areas now lie within the boundaries of the Tombstone Territorial Park and have been withdrawn from staking.
References
BREMNER, T.J., 1994. Proposed Tombstone Park: Preliminary Review of Mineral Potential. Exploration and Geological Services Division, Indian and Northern Affairs Canada. Open File 1994-2(T), 115 p.
CANADIAN UNITED MINERALS INC, Sep/98. Assessment Report #093930 by S. Ryan.
CANADIAN UNITED MINERALS INC, Sep/98. Assessment Report #093932 by S. Ryan.
THOMPSON, R.I., ROOTS, C.F. AND MUSTARD, P.S., 1992. Geology of Dawson map area (116B, C) (northeast of Tintina Trench); Geological Survey of Canada, Open File 2849 (13 sheets, scale: 1:50 000).
Work History
| Date | Work Type | Comment |
|---|---|---|
| 12/31/1998 | Ground Geophysics | |
| 12/31/1998 | Other |
Related References
| Number | Title | Page(s) | Reference Type | Document Type |
|---|---|---|---|---|
| ARMC016778 | Geochemical map - 116B/9 | Property File Collection | Geochemical Map |