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Text Description: Float boulder of silicic material at Site 1 in the Boyden Hills. Fine-grained, holocrystalline, porphyritic to glomeroporphyritic with a matrix of cryptocrystalline material, opaque and feldspar. Plagioclase phenocrysts (An55) are up to 1.88 mm and oscillatory zoning is common with less abundant normal zoning, grains occasionally have orthopyroxene or opaque inclusions. Orthopyroxene phenocrysts are up to 0.7 mm with intense pleochroism (birefringence is maximum for orthopyroxene), and frequently opaque inclusions are present. Amphibole phenocrysts are up to 1.3 mm with red-brown pleochroism and some have black coronas; occasionally grains have opaque inclusions; and some opaque aggregates may be dehydrated amphibole. Opaque phenocrysts are up to 0.3 mm. References: ![]() |
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 | |
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93SJP20 | 62.47407338 | -143.0635288 | Preece, S. J. | 1993-00-00 | Skookum Creek | Nabesna B-5; T8N, R13E, S18 | Float boulder of silicic material at Site 1 in the Boyden Hills. Fine-grained, holocrystalline, porphyritic to glomeroporphyritic with a matrix of cryptocrystalline material, opaque and feldspar. Plagioclase phenocrysts (An55) are up to 1.88 mm and oscillatory zoning is common with less abundant normal zoning, grains occasionally have orthopyroxene or opaque inclusions. Orthopyroxene phenocrysts are up to 0.7 mm with intense pleochroism (birefringence is maximum for orthopyroxene), and frequently opaque inclusions are present. Amphibole phenocrysts are up to 1.3 mm with red-brown pleochroism and some have black coronas; occasionally grains have opaque inclusions; and some opaque aggregates may be dehydrated amphibole. Opaque phenocrysts are up to 0.3 mm. | 93SJP20 | Lava | Whole-rock | 66.63 | 0.54 | 16.22 | 3.46 | 0.09 | 1.2 | 3.47 | 4.5 | 2.53 | 0.2 | 99.83 | 55 | DCP | 3.82 | 3.46 | LOI=1.12 | DCP | 47 | 858 | 402 | 18 | 207 | 6.7 | 6.2 | 2.8 | 6 | 47 | 14 | 3 | 5 | 55 | 16 | 55 | XRF: Rb, Zr, Nb, Th, U, Ni, Ga; DCP: Ba, Sc, V; MX: Sr, Y, Cr, Cu, Zn; |
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