Sample s_BCL-6
NavDat sample number 17069 · BASALT
Sample
| Sample ID | s_BCL-6 |
|---|---|
| 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 | 49.92 | WT% | XRF | |
| TIO2 | 1.34 | WT% | XRF | |
| AL2O3 | 16.49 | WT% | XRF | |
| FE2O3T | 11.21 | WT% | XRF | |
| CAO | 9.38 | WT% | XRF | |
| MGO | 7.67 | WT% | XRF | |
| MNO | 0.18 | WT% | XRF | |
| K2O | 0.58 | WT% | XRF | |
| NA2O | 2.69 | WT% | XRF | |
| P2O5 | 0.37 | WT% | XRF | |
| SC | 32 | PPM | XRF | |
| V | 246 | PPM | XRF | |
| CR | 149 | PPM | XRF | |
| NI | 132 | PPM | XRF | |
| CU | 99 | PPM | XRF | |
| ZN | 100 | PPM | XRF | |
| GA | 13 | PPM | XRF | |
| RB | 14 | PPM | XRF | |
| SR | 471 | PPM | XRF | |
| Y | 25 | PPM | XRF | |
| ZR | 130 | PPM | XRF | |
| NB | 5 | PPM | XRF | |
| BA | 398 | PPM | XRF | |
| LA | 10.7 | PPM | INAA | |
| CE | 28.7 | PPM | INAA | |
| SM | 4.01 | PPM | INAA | |
| EU | 1.47 | PPM | INAA | |
| TB | 0.75 | PPM | INAA | |
| YB | 2.62 | PPM | INAA | |
| LU | 0.36 | PPM | INAA | |
| SC | 27.1 | PPM | INAA | |
| CR | 137.4 | PPM | INAA | |
| CO | 43.3 | PPM | INAA | |
| BA | 345.8 | PPM | INAA | |
| HF | 2.48 | PPM | INAA | |
| TH | 0.56 | 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