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Sample JGM/R8C-27
NavDat sample number 85369
Sample
| Sample ID | JGM/R8C-27 |
|---|
| Material | notfound |
Location
| Latitude | 37.2154 |
|---|
| Longitude | -116.17 |
|---|
| 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 | 255.103 | | PPM | NAA |
| EU2O3 | 2.3459 | | PPM | NAA |
| HFO2 | 13.7137 | | PPM | NAA |
| LA2O3 | 162.193 | | PPM | NAA |
| LU2O3 | 0.2716 | | PPM | NAA |
| SC2O3 | 6.6664 | | PPM | NAA |
| SM2O3 | 9.1836 | | PPM | NAA |
| TB2O3 | | | PPM | NAA |
| THO2 | 37.3446 | | PPM | NAA |
| YB2O3 | 2.3469 | | PPM | NAA |
| AL2O3 | 16.22 | | WT% | XRF |
| BAO | 1906.95 | | PPM | XRF |
| BA | 1708 | | PPM | XRF |
| CAO | 1.9 | | WT% | XRF |
| CR2O3 | | | PPM | XRF |
| CR | | | PPM | XRF |
| CUO | | | PPM | XRF |
| FE2O3 | 2.423 | | WT% | XRF |
| K2O | 5.3 | | WT% | XRF |
| LA2O3 | 173.099 | | PPM | XRF |
| MGO | 0.66 | | WT% | XRF |
| MNO | 0.1033 | | WT% | XRF |
| MN | 0.08 | | WT% | XRF |
| NA2O | 4.35 | | WT% | XRF |
| NB2O5 | 29.4689 | | PPM | XRF |
| NIO | | | PPM | XRF |
| NI | | | PPM | XRF |
| P2O5 | 0.14 | | WT% | XRF |
| RB2O | 124.56 | | PPM | XRF |
| SIO2 | 65.63 | | WT% | XRF |
| SRO | 575.33 | | PPM | XRF |
| TIO2 | 0.47 | | WT% | XRF |
| TOTAL | 97.17 | | WT% | XRF |
| Y2O3 | | | PPM | XRF |
| ZNO | 86.757 | | PPM | XRF |
| ZN | 69.7 | | PPM | XRF |
| ZRO2 | 785.895 | | PPM | XRF |
| ZR | 581.8 | | 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