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Sample JGM/R11-3
NavDat sample number 85540
Sample
| Sample ID | JGM/R11-3 |
|---|
| Material | notfound |
|---|
Location
| Latitude | 37.1654 |
|---|
| Longitude | -116.286 |
|---|
| State / province | NEVADA |
|---|
Age
| Age (Ma) | Error | Min | Max | Geologic age | Dated by |
|---|
| 11.645 |
|
11.655 |
11.635 |
|
|
Analyses
Whole Rock
| Item | Value | Std. dev. | Unit | Method |
|---|
| CE2O3 | 79.9158 | | PPM | NAA |
| EU2O3 | | | PPM | NAA |
| HFO2 | 4.5469 | | PPM | NAA |
| LA2O3 | 29.9992 | | PPM | NAA |
| LU2O3 | 0.4008 | | PPM | NAA |
| SC2O3 | 8.5923 | | PPM | NAA |
| SM2O3 | 7.5022 | | PPM | NAA |
| TB2O3 | | | PPM | NAA |
| THO2 | 28.822 | | PPM | NAA |
| YB2O3 | 2.9048 | | PPM | NAA |
| AL2O3 | 12.53 | | WT% | XRF |
| BAO | | | PPM | XRF |
| BA | | | PPM | XRF |
| CAO | 0.67 | | WT% | XRF |
| CR2O3 | | | PPM | XRF |
| CR | | | PPM | XRF |
| CUO | | | PPM | XRF |
| FE2O3 | 0.5557 | | WT% | XRF |
| K2O | 6.39 | | WT% | XRF |
| LA2O3 | | | PPM | XRF |
| MGO | 0.25 | | WT% | XRF |
| MNO | 0.0646 | | WT% | XRF |
| MN | 0.05 | | WT% | XRF |
| NA2O | 2.41 | | WT% | XRF |
| NB2O5 | 64.0162 | | PPM | XRF |
| NIO | | | PPM | XRF |
| NI | | | PPM | XRF |
| P2O5 | 0.02 | | WT% | XRF |
| RB2O | 296.254 | | PPM | XRF |
| SIO2 | 73.97 | | WT% | XRF |
| SRO | | | PPM | XRF |
| TIO2 | 0.11 | | WT% | XRF |
| TOTAL | 96.96 | | WT% | XRF |
| Y2O3 | | | PPM | XRF |
| ZNO | 25.2554 | | PPM | XRF |
| ZN | 20.29 | | PPM | XRF |
| ZRO2 | 143.185 | | PPM | XRF |
| ZR | 106 | | PPM | XRF |
References
- Anonymous (1991) The Timber Mountain Tuff, southwestern Nevada volcanic field, U.S.A.; evidence against a long-lived, continuously evolving, zoned magma chamber. Eos, Transactions, American Geophysical Union, vol.72, no.17, pp.311, 23 Apr 1991
