|
Text Description: Sample from southwest flank 1,450’ asl. Porphyritic olivine basaltic andesite. Phenocrysts of plagioclase (20%, up to 0.8x 0.3 mm) and olivine (5%, 0.6–0.2 mm) in a groundmass of plagioclase laths (70 x 10 microns), smaller intersertal pyroxenes and opaque grains, and interstitial glass. This sample is one of very few collected from Vsevidof in 1988 that has plagioclase crystals with extensive spongy regions. They are typically throughout the crystals, with the exception of a thin (~ 20 micron) clear rim. 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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
88VS12 | 53.100150953755 | -168.73254480683 | Nye, C. J. | 1988-01-01 | Vsevidof | Sample from southwest flank 1,450’ asl. Porphyritic olivine basaltic andesite. Phenocrysts of plagioclase (20%, up to 0.8x 0.3 mm) and olivine (5%, 0.6–0.2 mm) in a groundmass of plagioclase laths (70 x 10 microns), smaller intersertal pyroxenes and opaque grains, and interstitial glass. This sample is one of very few collected from Vsevidof in 1988 that has plagioclase crystals with extensive spongy regions. They are typically throughout the crystals, with the exception of a thin (~ 20 micron) clear rim. | 88VS12 | Lava | Whole-rock | 53.88 | 1.181 | 17.73 | 0.159 | 5.29 | 8.88 | 3.2 | 0.874 | 0.221 | 100.65 | 13291 | XRF | 8.58 | 1.25 | 19 | 298 | 317 | 9 | 26 | 3.56034 | 16.38904 | 4.58 | 1.34242 | 5.00362 | 0.87 | 5.51 | 1.16 | 3.126 | 0.44 | 2.83 | 0.45 | 29 | 116 | 7 | 3.18508 | 0.61396 | 8 | 1 | 0.94726 | 29 | 245 | 37 | 27 | 125 | 82 | 21 | 13291 | ICPMS: Cs, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu, Hf, Ta, U; XRF: Rb, Ba, Sr, La, Ce, Y, Zr, Nb, Pb, Th, Sc, V, Cr, Ni, Cu, Zn, Ga; |
This website is supported by the U.S. Geological Survey under Cooperative Agreement Grant G22AC00137
Mention of trade names or commercial products does not constitute their endorsement by the U.S. Geological Survey.