Fluid Rare Earth Element Analyses from Geothermal Wells Located on the Reykjanes Peninsula, Iceland and Middle Valley Seafloor Hydrothermal System on the Juan de Fuca Ridge.
L o a d i n g
Owner
National Renewable Energy Laboratory (NREL) - view all
Update frequencyunknown
Last updatedabout 2 years ago
Format
OverviewAASG Geothermal DataGeothermal FluidHellisheidiHydrothermal FluidMiddle ValleyNGDS Content ModelNesjavellirREEReykjanesSvartsengiUSGIN Content Modelaqueous chemistrygeothermalmineral recoveryrare earth element
Results for fluid rare earth element analyses from four Reykjanes peninsula high-temperature geothermal fields. Data for fluids from hydrothermal vents located 2400 m below sea level from Middle Valley on the Juan de Fuca Ridge are also included. Data have been corrected for flashing. Samples preconcentrated using a chelating resin with IDA functional group (InertSep ME-1). Analyzed using an Element magnetic sector inductively coupled plasma mass spectrometry (ICP-MS).
Additional Information
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dcat_issued2015-05-01T06:00:00Z
dcat_modified2019-01-31T20:45:53Z
dcat_publisher_nameUniversity of California
guidhttps://data.openei.org/submissions/3505
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