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Text Description: A 4-5' thick, platy dike trending N25E that intrudes silicic rubble from Dome A near Site 5. Further up in the section, the dike flattens out to become a sill that intrudes into a lahar/pyroclastic flow package at Site 5. There is no bake zone with the lahar/pyroclastic flow. The sill then twists up vertically cutting through blocky autobrecciated? flows. Fine-grained, holocrystalline, intergranular, seriate porphyritic with matrix of mesostasis, red alteration patches, opaque, plagioclase and clinopyroxene. Plagioclase phenocrysts (An17-An49) are up to 1.8 mm and most large grains have sieve textured intermediate zones, complex zoning, and a few include orthopyroxene and matrix along rim. Orthopyroxene phenocrysts are up to 1.0 mm and display thick clinopyroxene rims, opaque and melt inclusions, and several have resorbed edges. 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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94SJP26 | 62.44 | -143.1263032 | Preece, S. J. | 1994-00-00 | Skookum Creek | Nabesna B-5, T8N, R12E, S26 | A 4-5' thick, platy dike trending N25E that intrudes silicic rubble from Dome A near Site 5. Further up in the section, the dike flattens out to become a sill that intrudes into a lahar/pyroclastic flow package at Site 5. There is no bake zone with the lahar/pyroclastic flow. The sill then twists up vertically cutting through blocky autobrecciated? flows. Fine-grained, holocrystalline, intergranular, seriate porphyritic with matrix of mesostasis, red alteration patches, opaque, plagioclase and clinopyroxene. Plagioclase phenocrysts (An17-An49) are up to 1.8 mm and most large grains have sieve textured intermediate zones, complex zoning, and a few include orthopyroxene and matrix along rim. Orthopyroxene phenocrysts are up to 1.0 mm and display thick clinopyroxene rims, opaque and melt inclusions, and several have resorbed edges. | 94SJP26 | Lava | Whole-rock | 57.36 | 0.86 | 17.97 | 5.57 | 0.12 | 4.36 | 7.26 | 3.9 | 1.5 | 0.37 | 98.8 | 55 | DCP | 6.08 | 5.57 | LOI=0.73 | DCP | 27 | 575 | 548 | 19 | 130 | 4.1 | 4.5 | 2.4 | 18.4 | 153 | 72 | 75 | 49 | 61 | 17.6 | 55 | XRF: Rb, Zr, Nb, Th, U, Ni, Ga; DCP: Ba, Sc, V; MX: Sr, Y, Cr, Cu, Zn; |
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