| Deposit ID | 10047413 |
|---|---|
| MRDS ID | M242713 |
| Record type | Site |
| Current site name | Tmb Associates Claims |
| Alternate or previous names | NBMG Sample Sites 476,477, Lake Range Mont Morillonite |
| Geographic coordinates: | -119.38879, 40.43349 (WGS84) |
|---|---|
| Elevation | 1402 |
Political divisions (FIPS codes)
Washoe(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
San Emidio Desert North(quadrangle 1:24,000 scale)
Kumiva Peak(quadrangle 1:100,000 scale)
Lovelock(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Smoke Creek Desert(hydrologic unit)
Black Rock Desert(hydrologic accounting unit)
Black Rock Desert-Humboldt(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 | Washoe |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 030N | 023E | 27,34, | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Clay | Secondary |
| Materials | Type of material |
|---|---|
| Gold | Ore |
| Montmorillonite | Ore |
| Chalcedony | Gangue |
| Result | SAMPLE 476 OF SELECTED FINELY LAMINATED SUBAQUEOUS SINTER CONTAINS 0.02% MG, 0.07% CA, 0.1% TI, 100 PPM MN, 5 PPM AG, 10 PPM B, 1000 PPM BA, 1.5 PPM BE, 20 PPM CU, 50 PPM LA, 100 PPM PB, 100 PPM SR, 20 PPM V, 30 PPM ZR. SAMPLE 477 OF REED-BEARING SINTER CONTAINS 0.02% MG, 0.07% CA, 20 PPM MN, 1.5 PPM AG, 50 PPM B, 500 PPM BA, 2 PPM BE, 10 PPM CU, 50 PPM LA, 100 PPM PB, 100 PPM SR, 20 PPM V, 10 PPM ZR. |
|---|
| Model code | 104 |
|---|---|
| USGS model code | 25a |
| Deposit model name | Hot-spring Au-Ag |
| Mark3 model number | 45 |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff | ||
| |||
| (1) | -119.38879, 40.43349 |
|---|
| Development status | Occurrence |
|---|---|
| Commodity type | Both |
| Deposit size | Small |
| Significant | No |
| District name | San Emidio Desert Area. |
|---|
| Ownership category | BLM Administrative Area |
|---|
| Type | Operator |
|---|---|
| Owner | Exploration Associates, Of Tucson |
| First year | 1979 |
| Type | Owner |
|---|---|
| Owner | Tmb Associates |
| First year | 1979 |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M242713 |
GARSIDE, L.J., 15 JUN 83, NBMG FIELD EXAMINATION AND SAMPLE ANALYSES.
BONHAM, H.F., JR., AND PAPKE, K.G., 1969, NBMG BULL 70, P.108-130.
GARSIDE, L.J. AND SCHILLING, J.M., 1979, THERMAL WATERS OF NEVADA; NBMG BULL. 91.
NBMG STAFF, 1985, NBMG OFR 85-3.
| Subject category | Comment text |
|---|---|
| Deposit | THE AREA HAS BEEN KNOWN FOR 15 YRS OR MORE TO CONTAIN SILICIFIED REEDS IN PLIOCENE SEDIMENTARY ROCKS AN AREA OF 2-3 SQ. KM. IN THE PLIOCENE TUFFACEOUS AND VOLCANICLASTIC SEDIMENTARY ROCKS IS ARGILLIZED AND SILICIFIED. UNALTERED EQUIVALENT? STRATA ARE EXPOSED TO THE EAST OF THE LONE MINERALIZED HILL. THE HILL APPEARS TO BE CAPPED BY STRONGLY SILICIFIED SEDIMENTS, WHICH ARE UNDERLAIN AND SURROUNDED? BY ARGILIZED ROCKS. THE SILICIFIED ROCKS CONSIST, IN PART, OF SYN DEPOSITIONAL SUBAQUEOUS SPRING SINTER, PROBABLY PRODUCED BY SUBLACUSTRINE, SILICA-CHARGED HOT SPRINGS WHICH VENTED DURING THE DEPOSITION OF THE PLIOCENE SEDIMENTS. IN ADDITION TO THE REED-BEARING SUBAQUEOUS SINTER, A VERY FINELY AND EVENLY LAMINATED SINTER IS INTERPRETED AS BEING SUBAQUEOUS ALSO. THE PLIOCENE SEDIMENTARY ROCKS ARE GENTLY DIPPING, AND IN THE SILICIFIED AREA CONTAIN IRREGULAR PODS AND LENSES (UP TO 0.5 M THICK) OF LIGHT TO DARK GREY CHALCEDONY, BELIEVED TO BE SINTER. A FEW SILICIFIED HYDROTHERMAL? |
| Deposit | BRECCIAS WERE NOTED. AT A PROSPECT SYMBOL SHOWN ON THE TOPOMAP APPROX. ON THE SEC 27/SEC28 LINE, ARGILLIZED, TUFFACEOUS SEDIMENTS (SMECTITE CLAYS AND SELENITE GYPSUM ARE PRESENT) ARE EXPOSED. THIS PROSPECT IS PROBABLY THE LAKE RANGE MONTMORILLONITE DESCRIBED BY PAPKE (1969, P.113). ARGILLIC ALTERATION PROBABLY RESULTED FROM HYDROTHERMAL ALTERATION DURING THE PERIOD OF HOT SPRING DISCHARGE IN THE PLIOCENE LAKE PRODUCING A SINTER CAP OVER ARGILLIZED SEDIMENTS. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUN-1986 | La Pointe, D.D. (Tingley, J.V.) | Nevada Bureau of Mines and Geology | |
| Updater | 01-SEP-1994 | Li, Zhiping (Peters, S.) | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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