Sample s_98-29
NavDat sample number 43354 · ANDESITE
Sample
| Sample ID | s_98-29 |
|---|---|
| Rock name | ANDESITE |
| Rock type | VOLCANIC |
| Composition | INTERMEDIATE |
| Material | IGNEOUS |
| Texture | PORPHYRITIC |
| Comment | UPPER UNIT |
Location
| Latitude | 46.87 |
|---|---|
| Longitude | -121.758 |
| Location | Burroughs Mountain Lava Flow |
| State / province | Washington |
| Location comment | North Vertical Section |
Age
| Age (Ma) | Error | Min | Max | Geologic age | Dated by |
|---|---|---|---|---|---|
| 0.496 | 0.489 | 0.503 |
Analyses
Whole rock
| Item | Value | Std. dev. | Unit | Method |
|---|---|---|---|---|
| SIO2 | 61.7 | WT% | XRF | |
| TIO2 | 0.96 | WT% | XRF | |
| AL2O3 | 16.4 | WT% | XRF | |
| FE2O3T | 6.47 | WT% | XRF | |
| CAO | 5.91 | WT% | XRF | |
| MGO | 3.58 | WT% | XRF | |
| MNO | 0.1 | WT% | XRF | |
| K2O | 1.65 | WT% | XRF | |
| NA2O | 3.98 | WT% | XRF | |
| P2O5 | 0.26 | WT% | XRF | |
| LA | 21.4 | PPM | LA-ICPMS | |
| CE | 46 | PPM | LA-ICPMS | |
| PR | 6.08 | PPM | LA-ICPMS | |
| ND | 24.2 | PPM | LA-ICPMS | |
| SM | 4.77 | PPM | LA-ICPMS | |
| EU | 1.41 | PPM | LA-ICPMS | |
| GD | 4.05 | PPM | LA-ICPMS | |
| TB | 0.61 | PPM | LA-ICPMS | |
| DY | 3.27 | PPM | LA-ICPMS | |
| HO | 0.63 | PPM | LA-ICPMS | |
| ER | 1.66 | PPM | LA-ICPMS | |
| YB | 1.61 | PPM | LA-ICPMS | |
| LU | 0.23 | PPM | LA-ICPMS | |
| V | 127 | PPM | LA-ICPMS | |
| CR | 82 | PPM | LA-ICPMS | |
| NI | 21 | PPM | XRF | |
| CU | 29 | PPM | XRF | |
| ZN | 74 | PPM | XRF | |
| RB | 36 | PPM | XRF | |
| SR | 587 | PPM | XRF | |
| Y | 17 | PPM | XRF | |
| ZR | 176 | PPM | XRF | |
| NB | 12 | PPM | LA-ICPMS | |
| BA | 435 | PPM | XRF | |
| HF | 4.79 | PPM | LA-ICPMS | |
| TA | 0.79 | PPM | LA-ICPMS | |
| PB | 9.6 | PPM | LA-ICPMS | |
| TH | 5.9 | PPM | LA-ICPMS | |
| U | 2.1 | PPM | LA-ICPMS |
References
- Stockstill, Karen R; Vogel, Thomas A; Sisson, Thomas W (2003) Origin and emplacement of the andesite of Burroughs Mountain, a zoned, large-volume lava flow at Mount Rainier, Washington, USA. Journal of Volcanology and Geothermal Research. 119; 1-4, Pages 275-296. 2003. doi:10.1016/S0377-0273(02)00358-X