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Copper Queen Mine, SFS Cu deposit (Longshot Ridge; Luning), Volcano Peak, Santa Fe District, Gabbs Valley Range, Mineral County, Nevada, USAi
Regional Level Types
Copper Queen MineMine
SFS Cu deposit (Longshot Ridge; Luning)Deposit
Volcano PeakPeak
Santa Fe DistrictMining District
Gabbs Valley RangeMountain Range
Mineral CountyCounty
NevadaState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
38° 34' 51'' North , 118° 5' 46'' West
Latitude & Longitude (decimal):
Type:
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Mina155 (2011)21.2km
Gabbs269 (2011)35.4km
Mindat Locality ID:
39779
Long-form identifier:
mindat:1:2:39779:6
GUID (UUID V4):
970ba915-64a4-4fb7-b017-d13915c292e1
Other/historical names associated with this locality:
Emma and St. Patrick claims; Mildred Claim


Deposit: Tactite zone between granitic rock and limestone containing oxide and carbonate copper minerals, As high As 8% cu locally. The copper ore is sporadically distributed.

Development: Claims extend for several thousand feet along a tactite zone

Geology: Mineralization within the New York Canyon property consists principally of contact metasomatic copper skarn deposits, porphyry-type copper-molybdenum mineralization, and a combination or transition of these two types of mineralization. The property's copper skarns may be almost entirely oxidized, as at Longshot Ridge, or consist of both oxide and sulphide skarns as at the Champion prospect, located midway between the Longshot Ridge and Copper Queen prospects. At Copper Queen, the mineralization consists of copper sulphide skarn and porphyry copper-molybdenum sulphide. Contact metasomatic skarn (also known as tactite) typically occurs in carbonate sedimentary rocks adjacent to small to moderate sized intrusive rock bodies of intermediate composition, such as monzonite and granodiorite. Heat and fluids from the intrusion recrystallize and alter the carbonate rocks, converting limestone and limy sediments to higher temperature calc-silicate minerals such as garnet, epidote, diopside, tremolite and calcite (Lindgren, 1913; Titley, 1995). A variety of metalliferous deposits can be formed, including those that are copper-rich, iron-rich or tungsten-rich.

Rock formation(s): Granitic Rocks
Luning


Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


4 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
β“˜Cuprite4.AA.10Cu2O
Group 5 - Nitrates and Carbonates
β“˜Malachite5.BA.10Cu2(CO3)(OH)2
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Conichalcite8.BH.35CaCu(AsO4)(OH)
Group 9 - Silicates
β“˜Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 Β· nH2O, x < 1

List of minerals for each chemical element

HHydrogen
Hβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Hβ“˜ ConichalciteCaCu(AsO4)(OH)
Hβ“˜ MalachiteCu2(CO3)(OH)2
CCarbon
Cβ“˜ MalachiteCu2(CO3)(OH)2
OOxygen
Oβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Oβ“˜ ConichalciteCaCu(AsO4)(OH)
Oβ“˜ CupriteCu2O
Oβ“˜ MalachiteCu2(CO3)(OH)2
AlAluminium
Alβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
SiSilicon
Siβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
CaCalcium
Caβ“˜ ConichalciteCaCu(AsO4)(OH)
CuCopper
Cuβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cuβ“˜ ConichalciteCaCu(AsO4)(OH)
Cuβ“˜ CupriteCu2O
Cuβ“˜ MalachiteCu2(CO3)(OH)2
AsArsenic
Asβ“˜ ConichalciteCaCu(AsO4)(OH)

Other Databases

Link to USGS MRDS:10045466

Other Regions, Features and Areas containing this locality


This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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