Sample 95ID-3B
NavDat sample number 38689 · BASALTIC-ANDESITE
Sample
| Sample ID | 95ID-3B |
|---|---|
| Rock name | BASALTIC-ANDESITE |
| Rock type | VOLCANIC |
| Composition | INTERMEDIATE |
| Material | IGNEOUS |
| Comment | fine grained, porphyritic with phenos of plag and pyrox; same locality as 95ID-3A but fresher |
Location
| Latitude | 44.3483 |
|---|---|
| Longitude | -114.265 |
| Location | Highway 75 |
| State / province | Idaho |
| Volcanic field | Tvs of main effusive phase, Challis Volcanic Group |
Age
| Age (Ma) | Error | Min | Max | Geologic age | Dated by |
|---|---|---|---|---|---|
| 49 | 48 | 50 |
Analyses
Whole rock
| Item | Value | Std. dev. | Unit | Method |
|---|---|---|---|---|
| SIO2 | 60.09 | WT% | XRF | |
| TIO2 | 1.2 | WT% | XRF | |
| AL2O3 | 16.74 | WT% | XRF | |
| FEOT | 5.63 | WT% | XRF | |
| MNO | 0.1 | WT% | XRF | |
| MGO | 2.37 | WT% | XRF | |
| CAO | 7.9 | WT% | XRF | |
| NA2O | 3.2 | WT% | XRF | |
| K2O | 2.38 | WT% | XRF | |
| P2O5 | 0.41 | WT% | XRF | |
| LOI | 5.19 | WT% | XRF | |
| TOTAL | 100 | WT% | XRF | |
| NI | 82 | PPM | XRF | |
| CR | 274 | PPM | XRF | |
| SC | 17 | PPM | XRF | |
| V | 129 | PPM | XRF | |
| GA | 22 | PPM | XRF | |
| CU | 15 | PPM | XRF | |
| ZN | 94 | PPM | XRF | |
| BA | 1220 | PPM | ICPMS | |
| RB | 50.8 | PPM | ICPMS | |
| SR | 759 | PPM | ICPMS | |
| U | 1.75 | PPM | ICPMS | |
| PB | 14.27 | PPM | ICPMS | |
| CS | 1.36 | PPM | ICPMS | |
| TH | 9.1 | PPM | ICPMS | |
| ZR | 260 | PPM | XRF | |
| Y | 21.54 | PPM | ICPMS | |
| NB | 22.1 | PPM | XRF | |
| HF | 7.2 | PPM | ICPMS | |
| TA | 1.03 | PPM | ICPMS | |
| LA | 62.32 | PPM | ICPMS | |
| CE | 108.61 | PPM | ICPMS | |
| PR | 11.71 | PPM | ICPMS | |
| ND | 44.24 | PPM | ICPMS | |
| SM | 8.52 | PPM | ICPMS | |
| EU | 2.29 | PPM | ICPMS | |
| GD | 6.28 | PPM | ICPMS | |
| TB | 0.88 | PPM | ICPMS | |
| DY | 4.57 | PPM | ICPMS | |
| HO | 0.82 | PPM | ICPMS | |
| ER | 2.02 | PPM | ICPMS | |
| TM | 0.28 | PPM | ICPMS | |
| YB | 1.72 | PPM | ICPMS | |
| LU | 0.26 | PPM | ICPMS | |
| SR87_SR86 | 0.70814 | TIMS |