| Deposit ID | 10037384 |
|---|---|
| MRDS ID | M032089 |
| Record type | Site |
| Current site name | Delamar Zinc |
| Alternate or previous names | North Star Claims, NBMG Sample Site 1745 |
| Related records | 10295404 |
| Geographic coordinates: | -114.79251, 37.51719 (WGS84) |
|---|---|
| Elevation | 1951 |
Political divisions (FIPS codes)
Lincoln(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Pahroc Spring SE(quadrangle 1:24,000 scale)
Caliente(quadrangle 1:100,000 scale)
Caliente(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Dry Lake Valley(hydrologic unit)
Central Nevada Desert Basins(hydrologic accounting unit)
Central Nevada Desert Basins(hydrologic subregion)
Great Basin(hydrologic region)
Federal lands
Bureau of Land Management(Bureau of Land Management NV)
Bureau of Land Management NV BLM(Type of land area)
BLM(Federal land areas administered by BLM)
| Country | State | County |
|---|---|---|
| United States | Nevada | Lincoln |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| 05S | 64E | 23 | Nevada |
| Commodity | Importance |
|---|---|
| Zinc Critical | Primary |
| Lead | Primary |
| Silver | Secondary |
| Manganese Critical | Secondary |
| Iron | Tertiary |
| Barium-Barite Critical | Tertiary |
| Copper | Tertiary |
| Strontium | Tertiary |
| Vanadium Critical | Tertiary |
| Cadmium | Tertiary |
| Molybdenum | Tertiary |
| Materials | Type of material |
|---|---|
| Smithsonite | Ore |
| Calcite | Gangue |
| Result | ORE RAN 15-30 % ZN AND 6 % PB. SAMPLE 1745 CONTAINS 20 000 PPM PB, 500 PPM SR, 200 PPM V, 5000 PPM ZN, 10 % FE, 15 % CA, GREATER THAN 5000 PPM MN, 100 PPM AG, 500 PPM BA, 200 PPM CD, 500 PPM CU, 50 PPM MO. |
|---|
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Unconsolidated Deposit > Silt | ||
| |||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone |
| (1) | -114.79251, 37.51719 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Abundant Normal Faults |
| General form | TABULAR |
|---|---|
| Thickness | 1.83M |
| Development status | Occurrence |
|---|---|
| Commodity type | Both |
| Deposit size | Small |
| Significant | No |
| District name | Delamar (Ferguson) District District |
|---|
| Ownership category | Private |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M032089 |
TSCHANZ, C.M., AND PAMPEYAN, E.H., 1970, GEOLOGY AND MINERAL DEPOSITS OF LINCOLN CO, NEV. NEV BUR MINES BULL 73 P. 141
CALLAGHAN, E., 1937, GEOLOGY OF THE DELAMAR DISTRICT, LINCOLN CO., NEV BUR MINES V. 31 NO. 5
BENTZ, J. AND SMITH, P., 1983, FIELD EXAMINATION REPORT, SEPT 22, 1983
| Subject category | Comment text |
|---|---|
| Deposit | SHAFTS SUNK ON A NE-STRIKING FAULT IN THE CHISHOLM SHALE AND ON A NW-STRIKING FAULT BETWEEN THE HIGHLAND PEAK LIMESTONE AND CHISHOLM SHALE. PRESENCE OF GOSSAN BRECCIA SUPPORTS A FAULT-RELATED ORIGIN. SHAFT NO. 1 (WESTERNMOST) EXPOSES A 2 FT WIDE REPLACEMENT VEIN WHICH PARALLELS THE BEDDING OF THE HOST LIMESTONE. THE VEIN STRIKES N40E, DIPS 60SE AND HAS A SHARP CONTACT WITH ENCLOSING HOST ROCK, WHICH APPEARS LITTLE ALTERED. VEIN IS COMPLETELY OXIDIZED, AND CONSISTS OF LIMONITIC AND MN-RICH GOSSAN WITH SOME CALCITE AND SILICA VEINING AND VUG FILLINGS. CALCITE (AND PROBABLY SOME SMITHSONITE) ALSO CEMENTS GOSSAN BRECCIA FOUND ON THE DUMP. THE GOSSAN IS QUITE DENSE AND MAY CONTAIN PB OR ZN MINERALS, BUT NO UNOXIDIZED MINERALS WERE OBSERVED. SHAFT NO. 2, (SOUTHERNMOST): UPPER SHAFT EXPLORES SIMILAR REPLACEMENT VEIN 5-6 FT WIDE STRIKING N30E, DIP 80SE. THE VEIN POSSIBLY PARALLELS THE BEDDING OR CROSSCUTS THE BEDDING AT A LOW ANGLE. THE GOSSAN "VEIN" IS NOT AS PURE OR HIGHGRADE AS THAT |
| Deposit | OBSERVED IN NO. 1. INSTEAD, IT IS SPOTTY, PINCHES OUT AND CONTAINS LIMESTONE LENSES ALONG FRACTURES PARALLEL TO BEDDING. SHAFT NO. 3 (NORTHERNMOST): LOWER SHAFT IS INCLINED ALONG STRIKE OF N10-20E (POORLY EXPOSED) TRENDING GOSSAN REPLACEMENT VEIN WHICH IS PROBABLY A CONTINUATION OF THE VEIN OBSERVED IN NO. 2. ADIT (OR INCLINE) LOCATED BELOW AND INTERSECTING THE SHAFT IS CAVED. DUMP CONSISTS OF LIMESTONE WASTE ROCK AND LIMONITIC MN-GOSSAN WHICH IN GENERAL IS LIGHT-WEIGHT, PUNKY, AND IN PART SILICEOUS. SAMPLE 1745 WAS TAKEN FROM THIS SHAFT. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-NOV-1979 | Harner, Joy L. (Roberts, Ralph J.) | U.S. Geological Survey | |
| Updater | 01-AUG-1984 | La Pointe, D.D. (Tingley, J.V.) | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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