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SAMPLE INFO : 05SMMC002
Sample ID:05SMMC002
Station ID:05SMMC002
Latitude:51.88123
Longitude:179.6023
Datum:NAD83
Date Sampled:2005-09-11
Sample Type 1:Lava
Field Lithology:Basalt
Final Unit:Sugarloaf Head
Text Description:
poorly vegetated lava flow margin near coast (from south sugarloaf satellite vent). Dense to wormy vesicles. Fine grained, plag-cpx-ol basalt, sparkly texture.

References:
Postglacial eruptive history and geochemistry of Semisopochnoi volcano, western Aleutian Islands, Alaska

GEOCHEM DATA
StationIDLatitudeLongitudeGeologistDateVisitedAge InfoVolcanoEruptionLocation DescriptionText DescriptionSample IDSample Type 1Sample Type 2Geologic 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
05SMMC00251.88123179.6023Coombs, M. L.2005-09-11 SemisopochnoiYoung lava flow from satellite cone on the west flank of the south sugarloafpoorly vegetated lava flow margin near coast (from south sugarloaf satellite vent). Dense to wormy vesicles. Fine grained, plag-cpx-ol basalt, sparkly texture.05SMMC002LavaSugarloaf HeadWhole-rock 53.09295604 1.048471773 18.90189124 9.0821772266087 0.228417819 3.73383402 8.423598322 3.942494773 1.2416084 0.304560443 99.4580913321XRF9.0821772266087 1.469300115 27.05924019 542.0566949 498.8446504 10.88196049 25.60692868 3.853746361 18.06697719 4.763745082 1.620843 4.808852996 0.779192723 4.776885489 0.978378345 2.738697483 0.393584534 2.384805373 0.378504773 24.3946726 84.96524152 2.059147516 2.532047415 0.124086973 6.353870414 1.847317461 0.918503371 20.33675496 13321ICPMS 27.3 541.1 503.8 15.1 28.5 19.3 25.2 91.1 2.9 6.7 1 22.9 231.6 2.3 4.8 95.6 18.413321XRF

SAMPLE LOCATION

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Page modified: August 1, 2017 15:29
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