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Text Description: Float boulder of silicic material at Site 1 in the Boyden Hills. Fine-grained, vesicular, holocrystalline, porphyritic to glomeroporphyritic with a matrix of cryptocrystalline material, opaque, feldspar and microlites. Cognate inclusions of equigranular masses of plagioclase, opaque, orthopyroxene and biotite are present. There is no melt reaction between the inclusion and the host. Plagioclase phenocrysts (An43 - An53) are up to 2.2 mm and both oscillatory and normal zoning are common. Orthopyroxene phenocrysts are up to 2.75 mm, with intense pleochroism (birefringence at maximum for orthopyroxene) and large opaque inclusions. Dehydrated amphibole is present as opaque aggregates. Opaque phenocrysts up to 1.55 mm (does not appear to be aggregate). Biotite phenocrysts are up to 0.2 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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93SJP21 | 62.4751846 | -143.0665843 | 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, vesicular, holocrystalline, porphyritic to glomeroporphyritic with a matrix of cryptocrystalline material, opaque, feldspar and microlites. Cognate inclusions of equigranular masses of plagioclase, opaque, orthopyroxene and biotite are present. There is no melt reaction between the inclusion and the host. Plagioclase phenocrysts (An43 - An53) are up to 2.2 mm and both oscillatory and normal zoning are common. Orthopyroxene phenocrysts are up to 2.75 mm, with intense pleochroism (birefringence at maximum for orthopyroxene) and large opaque inclusions. Dehydrated amphibole is present as opaque aggregates. Opaque phenocrysts up to 1.55 mm (does not appear to be aggregate). Biotite phenocrysts are up to 0.2 mm. | 93SJP21 | Lava | Whole-rock | 67.3 | 0.56 | 16.61 | 3.56 | 0.08 | 0.8 | 3.56 | 4.85 | 2.28 | 0.15 | 99.17 | 55 | DCP | 3.91 | 3.56 | LOI=0.23 | DCP | 46 | 869 | 405 | 18 | 199 | 6 | 5.3 | 2.6 | 5.7 | 39 | 1 | 6 | 8 | 52 | 16.3 | 55 | XRF: Rb, Zr, Nb, Th, U, Ni, Ga; DCP: Ba, Sc, V; MX: Sr, Y, Cr, Cu, Zn; |
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