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SAMPLE INFO : 51N23
Sample ID:51N23
Station ID:51N23
Latitude:51.947000000919
Longitude:177.37
Datum:NAD83
Date Sampled:1951-01-01
Sample Type 1:Countryrock
Sample Type 2:Plutonic
Field Lithology:Gabbro
Text Description:
Gabbro, Vega Bay formation: plagioclase zoned from labradorite to oligoclase, clinopyroxene and orthopyroxene.

References:
Geologic reconnaissance of Kiska Island, Aleutian Islands, Alaska

GEOCHEM DATA
StationIDLatitudeLongitudeGeologistDateVisitedVolcanoEruptionLocation DescriptionText DescriptionSample IDMaterialSiO2TiO2Al2O3FeOTMnOMgOCaONa2OK2OP2O5Total-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
51N2351.947000000919177.37Nelson, W. H.1951-01-01KiskaIn the vicinity of a saddle on the summit ridgeGabbro, Vega Bay formation: plagioclase zoned from labradorite to oligoclase, clinopyroxene and orthopyroxene.51N23Whole Rock 48.724145110582 0.78295906852604 20.236480540365 9.3975826600504 0.1606069884156 4.3263507504452 11.684158407235 2.4994462572178 0.45170715491887 0.060227620655849 100.09275NN4.675.16H2OM=0.22; H2OP=1.37; CO2=0.05NN 2.7 723 7 745XRFLi V=1, M=SPEC, R=275;F V=0.02, M=NN, R=275;K V=0.37, M=NN, R=745;Yb V=3, M=SPEC, R=275;Y V=40, M=SPEC, R=275;Zr V=10, M=SPEC, R=275;Co V=30, M=SPEC, R=275;Cr V=6, M=SPEC, R=275;Cu V=200, M=SPEC, R=275;Ga V=10, M=SPEC, R=275;Ni V=10, M=SPEC, R=275;Sc V=50, M=SPEC, R=275;V V=500, M=SPEC, R=275;
51N2351.947000000919177.37Nelson, W. H.1951-01-01KiskaIn the vicinity of a saddle on the summit ridgeGabbro, Vega Bay formation: plagioclase zoned from labradorite to oligoclase, clinopyroxene and orthopyroxene.51N23Whole Rock H2OM=0.22; H2OP=1.37; CO2=0.05NNBa V=100, M=SPEC, R=275;Rb V=<20, M=SPEC, R=275;Sr V=1000, M=SPEC, R=275;

SAMPLE LOCATION

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