Sample s_OSH-A
NavDat sample number 17059 · BASALT
Sample
| Sample ID | s_OSH-A |
|---|---|
| Rock name | BASALT |
| Rock type | VOLCANIC |
| Composition | MAFIC |
| Material | IGNEOUS |
Location
| Latitude | 44 |
|---|---|
| Longitude | -120 |
| Location | COLUMBIA RIVER BASALT PROVINCE / BLUE MOUNTAINS PROVINCE / BEAR CREEK BASALT |
| State / province | WASHINGTON |
| Location comment | BEAR CREEK AREA |
Age
| Age (Ma) | Error | Min | Max | Geologic age | Dated by |
|---|---|---|---|---|---|
| 12.8 | 1.8 | 23.8 |
Analyses
Whole rock
| Item | Value | Std. dev. | Unit | Method |
|---|---|---|---|---|
| SIO2 | 48.84 | WT% | XRF | |
| TIO2 | 0.63 | WT% | XRF | |
| AL2O3 | 16.98 | WT% | XRF | |
| FE2O3T | 9.06 | WT% | XRF | |
| CAO | 12.3 | WT% | XRF | |
| MGO | 9.9 | WT% | XRF | |
| MNO | 0.16 | WT% | XRF | |
| K2O | 0.16 | WT% | XRF | |
| NA2O | 1.8 | WT% | XRF | |
| P2O5 | 0.07 | WT% | XRF | |
| SC | 39 | PPM | XRF | |
| V | 228 | PPM | XRF | |
| CR | 230 | PPM | XRF | |
| NI | 128 | PPM | XRF | |
| CU | 102 | PPM | XRF | |
| ZN | 46 | PPM | XRF | |
| GA | 11 | PPM | XRF | |
| RB | 4 | PPM | XRF | |
| SR | 176 | PPM | XRF | |
| Y | 20 | PPM | XRF | |
| ZR | 48 | PPM | XRF | |
| BA | 94 | PPM | XRF | |
| LA | 2.85 | PPM | INAA | |
| CE | 8.72 | PPM | INAA | |
| SM | 1.59 | PPM | INAA | |
| EU | 0.69 | PPM | INAA | |
| TB | 0.4 | PPM | INAA | |
| YB | 2.35 | PPM | INAA | |
| LU | 0.33 | PPM | INAA | |
| SC | 35.9 | PPM | INAA | |
| CR | 205 | PPM | INAA | |
| CO | 40.9 | PPM | INAA | |
| BA | 93.9 | PPM | INAA | |
| HF | 1.05 | PPM | INAA | |
| TH | 0.28 | PPM | INAA |
References
- Brandon, Alan D (1989) Constraints on magma genesis behind the Neogene Cascade arc; evidence from major and trace element variation of high-alumina and tholeiitic volcanics of the Bear Creek area. Journal of Geophysical Research, B, Solid Earth and Planets. 94; 6, Pages 7775-7798. 1989. doi:10.1029/JB094iB06p07775