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Text Description: CG -Chetaslina Gl high-Sr- of Nye (1983). References:  Petrology and geochemistry of Okmok and Wrangell volcanoes, Alaska Geochemistry of some Quaternary lavas from the Aleutian Arc and Mt. Wrangell |
| StationID | Latitude | Longitude | Geologist | DateVisited | Age Info | Volcano | Eruption | Location Description | Text Description | Sample ID | Sample Type 1 | Sample Type 2 | Final Unit | Material | SiO2 | TiO2 | Al2O3 | FeOT | MnO | MgO | CaO | Na2O | K2O | P2O5 | Total-majors | REF majors | METH majors | Fe2O3/Fe203T orig | FeO/FeOT orig | Volatiles csv | METH volatiles | Cs | Rb | Ba | Sr | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | Y | Zr | Nb | Hf | Ta | Pb | Th | U | Sc | V | Cr | Fe | Co | Ni | Cu | Zn | Ga | Mo | As | Na | K | Ref trace1 | METH trace1 | Rb | Ba | Sr | La | Ce | Nd | Sm | Eu | Gd | Dy | Er | Yb | Lu | Y | Zr | Nb | Pb | Th | U | Sc | Ti | V | Cr | Ni | Cu | Zn | Ga | Ref trace2 | METH trace2 | Light csv | Halogen csv | other major csv | other lile csv | other ree csv | other hfse csv | other hpe csv | other tm csv | other misc csv | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 79cne17 | 61.9692 | -144.301 | Nye, C. J. | 1979-01-01 | Wrangell | The single largest continuous stratigraphic section exposed on Mt. Wrangell holds up the ridge immediately north of the Chetaslina Glacier. Samples 79cne01-79cne29 are superposed flows collected from altitudes between 4500 and 7500 ft. on a spur off the larger ridge. * * * Larger numbers are further upsection. | CG -Chetaslina Gl high-Sr- of Nye (1983). | 79cne17 | Lava | Whole-rock | 60.87 | 0.851 | 16.63 | 0.101 | 3.81 | 6.39 | 3.71 | 1.93 | 0.199 | 99.89 | 13291 | XRF | 5.5 | 0.612553575 | 41.06671485 | 622 | 717.3681453 | 16 | 40 | 4.674027359 | 18 | 3.906250992 | 1.142472751 | 3.685587807 | 0.595677266 | 3.536540464 | 0.72421988 | 1.91265445 | 0.272654798 | 1.71153931 | 0.271851607 | 18.07574477 | 156.9046985 | 5.084413571 | 4.306954712 | 0.384473451 | 8 | 5 | 1.516372536 | 17 | 159 | 66 | 0 | 58 | 63 | 19 | 13291 | ICPMS: Cs, Rb, Sr, Pr, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu, Y, Zr, Nb, Hf, Ta, U; XRF: Ba, La, Ce, Nd, Pb, Th, Sc, V, Cr, Cu, Zn, Ga; | |||||||||||||||||||||||||||||||||||||||||||||||||||||
| 79cne17 | 61.9692 | -144.301 | Nye, C. J. | 1979-01-01 | Wrangell | The single largest continuous stratigraphic section exposed on Mt. Wrangell holds up the ridge immediately north of the Chetaslina Glacier. Samples 79cne01-79cne29 are superposed flows collected from altitudes between 4500 and 7500 ft. on a spur off the larger ridge. * * * Larger numbers are further upsection. | CG -Chetaslina Gl high-Sr- of Nye (1983). | 79cne17 | Lava | Whole-rock | 59.79 | 0.83 | 16.45 | 0.11 | 3.91 | 6.44 | 4.1 | 1.9 | 0.2 | 100.36 | 47 | XRF | 6.28 | LOI=0.04 | XRF | 43 | 715 | 20 | 182 | 7.9 | 35 | 15856 | 47 | XRF |
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