| Deposit ID | 10046507 |
|---|---|
| MRDS ID | M241677 |
| Record type | Site |
| Current site name | NBMG Sample Site 1710 |
| Related records | 10149708 |
| Geographic coordinates: | -114.0825, 37.92302 (WGS84) |
|---|---|
| Elevation | 2146 |
Political divisions (FIPS codes)
Lincoln(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Deer Lodge Canyon(quadrangle 1:24,000 scale)
Caliente(quadrangle 1:100,000 scale)
Caliente(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Meadow Valley Wash(hydrologic unit)
Lower Colorado-Lake Mead(hydrologic accounting unit)
Lower Colorado-Lake Mead(hydrologic subregion)
Lower Colorado(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Nevada | Lincoln |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 001N | 070E | 25 | NE OF NE | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Primary |
| Barium-Barite Critical | Secondary |
| Fluorine-Fluorite Critical | Secondary |
| Materials | Type of material |
|---|---|
| Barite | Ore |
| Fluorite | Ore |
| Calcite | Gangue |
| Quartz | Gangue |
| Result | SAMPLE 1710 CONTAINS 100 PPM MN, 7 PPM AG, 150 PPM BA, 20 PPM PB. |
|---|
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Latite |
| (1) | -114.0825, 37.92302 |
|---|
| Type of structure | Local |
|---|---|
| Structure description | Shear Zone, Brecciation |
| General form | TABULAR |
|---|---|
| Strike | N30E |
| Dip | 75 SE |
| Thickness | 1.22M |
| Development status | Occurrence |
|---|---|
| Commodity type | Both |
| Deposit size | Small |
| Significant | No |
| District name | Eagle Valley (Fay) District |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M241677 |
BENTZ, J. AND SMITH, J., 1983, FIELD EXAMINATION REPORT, SEPT. 14, 1983
| Subject category | Comment text |
|---|---|
| Deposit | A PROMINENT RIB OF BANDED, FISSURE AND COCKSCOMB TYPE QUARTZ VEIN OUTCROPS AT SOUTH EDGE OF CAVED SHAFT. ENTIRE RIB IS COMPOSED OF SEVERAL BANDED, IRON-STAINED SUB-PARALLEL QUARTZ VEINS WHICH TOGETHER FORM A TOTAL VEIN OUTCROP WIDTH OF 3-4 FT. PRISMATIC COMB QUARTZ FORMS THE MID-PORTION OF VEIN OUTCROP WHILE MASSIVE TO CRUDELY BANDED WHITE, FE-STAINED QUARTZ COMPRISES REST OF VEIN. QUARTZ AFTER CALCITE LAMINAE ARE COMMON IN MORE MASSIVE WHITE VEIN MATERIAL. LATITE HOST IS SHEARED ON BOTH SIDES OF VEIN DUE TO FORCIBLE INTRUSION OF VEIN. ALSO SOME PORTIONS OF VEIN APPEAR BRECCIATED AND RECEMENTED BY QUARTZ. MASSIVE TO BANDED, PRISMATIC TO SUGARY, WHITE QUARTZ VEIN MATERIAL FROM DUMP CONTAINS OXIDIZED PYRITE AND POSSIBLY MINOR MAGNETITE. SOME CLEAR TO PINK FLUORITE POSSIBLY INTERGROWN WITH VEIN MATERIAL OR COATING VUGS. ALSO SOME VEIN MATERIAL IS HEAVY AND MAY CONTAIN BARITE. ROCK IS VUGGY AND IRON-STAINED. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-FEB-1984 | La Pointe, D.D. (Tingley, J.V.) | Nevada Bureau of Mines and Geology |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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