Sample 90TF098
NavDat sample number 51270 · GRANITE
Sample
| Sample ID | 90TF098 |
|---|---|
| Rock name | GRANITE |
| Rock type | PLUTONIC |
| Composition | FELSIC |
| Material | IGNEOUS |
| Collected by | Tom Frost |
| Comment | pluton |
Location
| Latitude | 46.5319 |
|---|---|
| Longitude | -115.057 |
| State / province | Idaho |
| Volcanic field | Horseshoe Lake stock |
Age
| Age (Ma) | Error | Min | Max | Geologic age | Dated by |
|---|---|---|---|---|---|
| 48 | 44 | 52 |
Analyses
Whole rock
| Item | Value | Std. dev. | Unit | Method |
|---|---|---|---|---|
| SIO2 | 75.93 | WT% | XRF | |
| TIO2 | 0.09 | WT% | XRF | |
| AL2O3 | 13.35 | WT% | XRF | |
| FEOT | 1.09 | WT% | XRF | |
| MNO | 0.01 | WT% | XRF | |
| MGO | 0.15 | WT% | XRF | |
| CAO | 0.59 | WT% | XRF | |
| NA2O | 4.19 | WT% | XRF | |
| K2O | 4.57 | WT% | XRF | |
| P2O5 | 0.03 | WT% | XRF | |
| BA | 209 | PPM | INAA | |
| SR | 59 | PPM | INAA | |
| CO | 0.62 | PPM | INAA | |
| NI | 3.6 | PPM | INAA | |
| CR | 1 | PPM | INAA | |
| CS | 5.24 | PPM | INAA | |
| HF | 6.84 | PPM | INAA | |
| RB | 188 | PPM | INAA | |
| SB | 0.04 | PPM | INAA | |
| TA | 2.93 | PPM | INAA | |
| TH | 23.5 | PPM | INAA | |
| U | 7.94 | PPM | INAA | |
| ZN | 40.3 | PPM | INAA | |
| ZR | 182 | PPM | INAA | |
| SC | 1.55 | PPM | INAA | |
| LA | 30.1 | PPM | INAA | |
| CE | 67.7 | PPM | INAA | |
| ND | 31.1 | PPM | INAA | |
| SM | 6.68 | PPM | INAA | |
| EU | 0.26 | PPM | INAA | |
| GD | 6.65 | PPM | INAA | |
| TB | 0.899 | PPM | INAA | |
| TM | 0.498 | PPM | INAA | |
| YB | 3.02 | PPM | INAA | |
| LU | 0.436 | PPM | INAA | |
| W | 1.1 | PPM | XRF | |
| NI | -10 | PPM | XRF | |
| CR | -20 | PPM | XRF | |
| BA | 210 | PPM | XRF | |
| RB | 160 | PPM | XRF | |
| SR | 56 | PPM | XRF | |
| ZR | 138 | PPM | XRF | |
| Y | 25 | PPM | XRF | |
| NB | 30 | PPM | XRF | |
| CU | -10 | PPM | XRF | |
| ZN | 50 | PPM | XRF | |
| LA | -30 | PPM | XRF | |
| CE | 69 | PPM | XRF | |
| RB | 189 | PPM | MS-ID | |
| SR | 60.3 | PPM | MS-ID | |
| RB87_SR86 | 9.07393 | TIMS | ||
| SR87_SR86 | 0.71393 | TIMS |