Sample OAB 42-82
NavDat sample number 31671 · BASALT
Sample
| Sample ID | OAB 42-82 |
|---|---|
| Rock name | BASALT |
| Rock type | VOLCANIC |
| Composition | MAFIC |
| Material | IGNEOUS |
| Comment | Stack of flows related to at least two vents. |
Location
| Latitude | 36.0769 |
|---|---|
| Longitude | -114.596 |
| Location | Petroglyph Wash |
| State / province | Arizona |
| Volcanic field | Lake Mead area |
Age
| Age (Ma) | Error | Min | Max | Geologic age | Dated by |
|---|---|---|---|---|---|
| 5.02 | 4.61 | 5.43 |
Analyses
Whole rock
| Item | Value | Std. dev. | Unit | Method |
|---|---|---|---|---|
| SIO2 | 47.52 | WT% | ICP | |
| AL2O3 | 16.61 | WT% | ICP | |
| FEO | 10.56 | WT% | ICP | |
| CAO | 9.79 | WT% | ICP | |
| MGO | 5.35 | WT% | ICP | |
| NA2O | 3.57 | WT% | ICP | |
| K2O | 2.11 | WT% | ICP | |
| TIO2 | 1.76 | WT% | ICP | |
| MNO | 0.16 | WT% | ICP | |
| P2O5 | 0.57 | WT% | ICP | |
| CR | 50 | PPM | INAA | |
| CO | 32 | PPM | INAA | |
| SC | 25 | PPM | INAA | |
| V | 281 | PPM | INAA | |
| HF | 4 | PPM | INAA | |
| TH | 5.28 | PPM | INAA | |
| TA | 1.87 | PPM | INAA | |
| LA | 37.7 | PPM | INAA | |
| CE | 72.3 | PPM | INAA | |
| SM | 6.2 | PPM | INAA | |
| EU | 1.6 | PPM | INAA | |
| YB | 2.5 | PPM | INAA | |
| LU | 0.4 | PPM | INAA | |
| SR | 598 | PPM | AAS | |
| RB | 22 | PPM | AAS | |
| BA | 800 | PPM | AAS | |
| NI | 30 | PPM | AAS | |
| NB | 34 | PPM | XRF | |
| ZR | 155 | PPM | XRF | |
| SR | 597.57 | PPM | MS-ID | |
| RB | 22.13 | PPM | MS-ID | |
| ND | 32.26 | PPM | MS-ID | |
| ND143_ND144 | 0.512603 | MS | ||
| SR87_SR86_INITIAL | 0.70555 | MS | ||
| PB206_PB204 | 18.263 | MS | ||
| PB207_PB204 | 15.548 | MS | ||
| PB208_PB204 | 38.397 | MS |
References
- Feuerbach, Dan L; Smith, Eugene I; Walker, J D; Tangeman, J A (1993) The role of the mantle during crustal extension; constraints from geochemistry of volcanic rocks in the Lake Mead area, Nevada and Arizona. Geological Society of America Bulletin, vol.105, no.12, pp.1561-1575, Dec 1993 doi:10.1130/0016-7606(1993)105<1561:TROTMD>2.3.CO;2