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SAMPLE INFO : id-25w
Sample ID:id-25w
Station ID:id-25
Latitude:53.41587
Longitude:-167.93727
Datum:NAD83
Date Sampled:1980-00-00
Sample Type 1:Lava
Final Unit:Pfm
 Text Description:
QTam sample from just N of Magazine Ridge. Original data in Nye, 1983 and Nye and Reid, 1986.

References:
Petrology and geochemistry of Okmok and Wrangell volcanoes, Alaska
Geochemistry of primary and least fractionated lavas from Okmok volcano, Central Aleutians: implications for arc magmagenesis
Geochemistry of some Quaternary lavas from the Aleutian Arc and Mt. Wrangell

GEOCHEM DATA
StationIDLatitudeLongitudeGeologistDateVisitedAge InfoVolcanoEruptionLocation DescriptionText DescriptionSample IDSample Type 1Sample Type 2Final UnitMaterialSiO2TiO2Al2O3FeOTMnOMgOCaONa2OK2OP2O5Total-majorsREF majorsMETH majorsFe2O3/Fe203T origFeO/FeOT origVolatiles csvMETH volatilesCsRbBaSrLaCePrNdSmEuGdTbDyHoErTmYbLuYZrNbHfTaPbThUScVCrFeCoNiCuZnGaMoAsNaKRef trace1METH trace1RbBaSrLaCeNdSmEuGdDyErYbLuYZrNbPbThUScTiVCrNiCuZnGaRef trace2METH trace2Light csvHalogen csvother major csvother lile csvother ree csvother hfse csvother hpe csvother tm csvother misc csv
id-2553.41587-167.93727Nye, C. J.1980-01-01 OkmokLatitude and longitude determined using Google Earth.QTam sample from just N of Magazine Ridge. Original data in Nye, 1983 and Nye and Reid, 1986.id-25wLavaPfmWhole-rock 49.57141696 0.665217745 18.17923302 7.982612935 0.15640234 8.317760806 12.2481313 2.254631134 0.517955801 0.106637959 98.46413291XRF7.982612935 0.283631883 9.257659218 173.6452201 449.4380023 4.711097747 10.25152623 1.647944393 7.022099295 1.974509348 0.752815037 2.150468363 0.378649764 2.328867356 0.487383822 1.364827907 0.194527457 1.234822096 0.195330319 11.86485806 35.64135958 0.980787024 1.110137045 0.073666164 2.347206492 0.951635572 0.471088909 35.83622379 236 211 73 86 61 18 13291ICPMS: 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; XRF: V, Cr, Ni, Cu, Zn, Ga;

SAMPLE LOCATION

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Page modified: August 1, 2017 15:29
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