Sample CBC87-110
NavDat sample number 20725 · GRANODIORITE
Sample
| Sample ID | CBC87-110 |
|---|---|
| Rock name | GRANODIORITE |
| Rock type | PLUTONIC |
| Composition | INTERMEDIATE |
| Material | IGNEOUS |
| Collected by | C.B. Clarke |
Location
| Latitude | 44.0653 |
|---|---|
| Longitude | -115.711 |
| Location | Long Gulch pluton traverse, South Fork of the Payette River |
| State / province | Idaho |
| Volcanic field | Idaho Batholith, Atlanta Lobe |
Age
| Age (Ma) | Error | Min | Max | Geologic age | Dated by |
|---|---|---|---|---|---|
| 78 | 72 | 85 |
Analyses
Whole rock
| Item | Value | Std. dev. | Unit | Method |
|---|---|---|---|---|
| SIO2 | 73.32 | WT% | EDXRF | |
| AL2O3 | 14.88 | WT% | EDXRF | |
| TIO2 | 0.14 | WT% | EDXRF | |
| FE2O3T | 1.18 | WT% | EDXRF | |
| MGO | 0.26 | WT% | EDXRF | |
| CAO | 1.37 | WT% | EDXRF | |
| NA2O | 4.38 | WT% | EDXRF | |
| K2O | 3.78 | WT% | EDXRF | |
| MNO | 0.04 | WT% | EDXRF | |
| P2O5 | 0.03 | WT% | EDXRF | |
| LOI | 0.54 | WT% | EDXRF | |
| TOTAL | 99.91 | WT% | EDXRF | |
| BA | 1710 | PPM | EDXRF | |
| CE | 7 | PPM | EDXRF | |
| CO | 7 | PPM | EDXRF | |
| CR | 8 | PPM | EDXRF | |
| CU | 1 | PPM | EDXRF | |
| LA | 21 | PPM | EDXRF | |
| NB | 18 | PPM | EDXRF | |
| ND | 12 | PPM | EDXRF | |
| NI | 2 | PPM | EDXRF | |
| PB | 17 | PPM | EDXRF | |
| RB | 87 | PPM | EDXRF | |
| SM | 7 | PPM | EDXRF | |
| SR | 609 | PPM | EDXRF | |
| TH | 9 | PPM | EDXRF | |
| U | 1 | PPM | EDXRF | |
| V | 12 | PPM | EDXRF | |
| ZN | 50 | PPM | EDXRF | |
| ZR | 95 | PPM | EDXRF | |
| Y | 8 | PPM | EDXRF | |
| LA | 35.09 | PPM | INAA | |
| CE | 61.36 | PPM | INAA | |
| ND | 23.11 | PPM | INAA | |
| SM | 3.773 | PPM | INAA | |
| EU | 1.059 | PPM | INAA | |
| GD | 5.061 | PPM | INAA | |
| TB | 0.3663 | PPM | INAA | |
| YB | 0.7008 | PPM | INAA | |
| LU | 0.1244 | PPM | INAA | |
| TH | 6.967 | PPM | INAA | |
| U | 1.635 | PPM | INAA | |
| TA | 0.8643 | PPM | INAA | |
| HF | 3.871 | PPM | INAA | |
| CS | 2.515 | PPM | INAA | |
| SR87_SR86 | 0.70936 | TIMS | ||
| ND143_ND144 | 0.51198 | TIMS |