Curly Kidney

Prospect, Inactive

Commodities and mineralogy

Main commodities Au
Ore minerals arsenopyrite; gold; pyrite
Gangue minerals carbonate minerals; chlorite; quartz; white mica

Geographic location

Quadrangle map, 1:250,000-scale VA
Quadrangle map, 1:63,360-scale A-7
Latitude 61.0092
Longitude -146.6014
Nearby scientific data Find additional scientific data near this location
Location and accuracy This prospect is on the crest of a north-northwest trending ridge, about 1 mile southeast of a small bay on the south side of Jack Bay. It is at an elevation of 1,500 feet in the NW1/4 section 14, T. 10 S., R. 8 W., of the Copper River Meridian. This prospect is probably located to within one-half mile. It is locality 39 of Cobb and Matson (1972) and locality 31 of Winkler and others (1981 [OFR 80-892-B]).

Geologic setting

Geologic description

Gold-bearing quartz veins occur in shear zones that cut metaflysch of the Valdez Group at this locality (Johnson, 1919; Winkler and others, 1981 [OFR 80-892-A]). The shear zones are as much as 10 feet wide and include as much as 3 feet of quartz stringers and lenses. The quartz contains pyrite and arsenopyrite. One shear was explored with at 25-foot-long adit (Johnson, 1919). The quartz veins are probably similar to other gold-bearing quartz veins cutting metaflysch of the Valdez Group in the southern Valdez quadrangle. Data summarized by Goldfarb and others (1997) show that gold-bearing quartz veins in the Valdez Group commonly contain pyrite, arsenopyrite, carbonate minerals, chlorite, and white mica and formed from water-rich fluids with 5 to 15 mole percent CO2 and significant amounts of CH4, N2, and H2S. The vein-forming fluid salinities were less than 8 percent, vein formation temperatures ranged from 225 to 375 degrees centigrade, and emplacement depths varied from 3 to 10 kilometers. The vein-forming fluids were produced by metamorphic devolatilization reactions. Radiometric dating indicates that the veins formed from 57 to 49 Ma (Goldfarb and others, 1997, p. 171), when deep parts of the accreted Valdez Group flysch underwent high-grade metamorphism and partial melting (Hudson, 1994).
Geologic map unit (-146.603421090015, 61.008666665393)
Mineral deposit model Low-sulfide Au-quartz veins (Cox and Singer, 1986; model 36a)
Mineral deposit model number 36a
Age of mineralization Radiometric dating indicates that the gold-bearing quartz veins in the Valdez Group formed from 57 to 49 Ma (Goldfarb and others, 1997, p. 171), when deep parts of the accreted Valdez Group flysch underwent high-grade metamorphism and partial melting (Hudson, 1994).
Alteration of deposit Country rocks to gold-bearing quartz veins in Valdez Group metaflysch can be variably silicified, carbonitized, and sericitized (Goldfarb and others, 1997).

Production and reserves

Workings or exploration One shear was explored with at 25-foot-long adit (Johnson, 1919).
Indication of production None

References