Sample 90TF053
NavDat sample number 49650 · GRANODIORITE
Sample
| Sample ID | 90TF053 |
|---|---|
| Rock name | GRANODIORITE |
| Rock type | PLUTONIC |
| Composition | INTERMEDIATE |
| Material | IGNEOUS |
| Collected by | Tom Frost |
Location
| Latitude | 46.8395 |
|---|---|
| Longitude | -115.62 |
| State / province | Idaho |
| Volcanic field | Beaver Creek pluton |
Age
| Age (Ma) | Error | Min | Max | Geologic age | Dated by |
|---|---|---|---|---|---|
| 48 | 44 | 52 |
Analyses
Whole rock
| Item | Value | Std. dev. | Unit | Method |
|---|---|---|---|---|
| SIO2 | 67.3 | WT% | XRF | |
| TIO2 | 0.5 | WT% | XRF | |
| AL2O3 | 15.6 | WT% | XRF | |
| FEOT | 2.86 | WT% | XRF | |
| MNO | 0.04 | WT% | XRF | |
| MGO | 1.31 | WT% | XRF | |
| CAO | 3.17 | WT% | XRF | |
| NA2O | 3.69 | WT% | XRF | |
| K2O | 3.92 | WT% | XRF | |
| P2O5 | 0.22 | WT% | XRF | |
| TOTAL | 98.61 | WT% | XRF | |
| H2O | 0.54 | WT% | UNKNOWN | |
| CO2 | -0.01 | WT% | UNKNOWN | |
| LOI | 0.33 | WT% | XRF | |
| FEO | 2.2 | WT% | TIT | |
| FE2O3 | 0.74 | WT% | TIT | |
| NI | -10 | PPM | XRF | |
| CR | -20 | PPM | XRF | |
| BA | 820 | PPM | XRF | |
| RB | 124 | PPM | XRF | |
| SR | 215 | PPM | XRF | |
| ZR | 194 | PPM | XRF | |
| Y | 25 | PPM | XRF | |
| NB | 12 | PPM | XRF | |
| CU | -10 | PPM | XRF | |
| ZN | 38 | PPM | XRF | |
| LA | 39 | PPM | XRF | |
| CE | 89 | PPM | XRF | |
| BA | 836 | PPM | INAA | |
| SR | 220 | PPM | INAA | |
| CO | 2.84 | PPM | INAA | |
| CR | 5.7 | PPM | INAA | |
| CS | 6.88 | PPM | INAA | |
| HF | 5.8 | PPM | INAA | |
| RB | 136 | PPM | INAA | |
| SB | 0.06 | PPM | INAA | |
| TA | 0.85 | PPM | INAA | |
| TH | 20.9 | PPM | INAA | |
| U | 3.36 | PPM | INAA | |
| ZN | 30 | PPM | INAA | |
| ZR | 213 | PPM | INAA | |
| SC | 3.4 | PPM | INAA | |
| LA | 43.4 | PPM | INAA | |
| CE | 87.8 | PPM | INAA | |
| ND | 33.8 | PPM | INAA | |
| SM | 6.05 | PPM | INAA | |
| EU | 0.76 | PPM | INAA | |
| GD | 4.93 | PPM | INAA | |
| TB | 0.603 | PPM | INAA | |
| TM | 0.267 | PPM | INAA | |
| YB | 1.67 | PPM | INAA | |
| LU | 0.237 | PPM | INAA |