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Text Description: CG -Chetaslina Gl homogeneous- 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 | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 79cne20 | 61.970176 | -144.3008 | 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 homogeneous- of Nye (1983). | 79cne20 | Lava | Whole-rock | 62.41 | 0.928 | 16.39 | 0.092 | 3.13 | 5.47 | 4.01 | 2.091 | 0.213 | 100.07 | 13291 | XRF | 5.26 | 1.046680504 | 49.13017317 | 604 | 538.6970316 | 18 | 44 | 4.973016242 | 20 | 4.358090977 | 1.184505081 | 4.217988951 | 0.674750323 | 4.075936068 | 0.823135375 | 2.186081622 | 0.318599926 | 1.920755508 | 0.305668742 | 20.52573465 | 187.5540417 | 6.07768857 | 5.133978795 | 0.466425844 | 7 | 5 | 1.729318084 | 16 | 139 | 42 | 0 | 59 | 62 | 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; | |||||||||||||||||||||||||||||||||||||||||||||||||||||
| 79cne20 | 61.970176 | -144.3008 | 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 homogeneous- of Nye (1983). | 79cne20 | Lava | Whole-rock | 61.52 | 0.88 | 16.4 | 0.1 | 3.19 | 5.59 | 4.26 | 2.05 | 0.22 | 100.12 | 47 | XRF | 5.8 | LOI=0.09 | XRF | 52 | 517 | 24 | 215 | 9.1 | 44 | 17018 | 47 | XRF |
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