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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.
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).
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Complete Metadata
| @type | dcat:Dataset |
|---|---|
| accessLevel | public |
| bureauCode |
[ "019:20" ] |
| contactPoint |
{ "fn": "Andrew Fowler", "@type": "vcard:Contact", "hasEmail": "mailto:apfowler@ucdavis.edu" } |
| dataQuality |
true
|
| description | 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). |
| distribution |
[ { "@type": "dcat:Distribution", "title": "Iceland Geothermal Fluid REE.xls", "format": "xls", "accessURL": "https://gdr.openei.org/files/803/Iceland%20Geothermal%20Fluid%20REE.xls", "mediaType": "application/vnd.ms-excel", "description": "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 ICP-MS. Formatted as the AASG Aqueous Chemistry Content Model" } ] |
| DOI | 10.15121/1261975 |
| identifier | https://data.openei.org/submissions/6996 |
| issued | 2015-05-01T06:00:00Z |
| keyword |
[ "AASG Geothermal Data", "Geothermal Fluid", "Hellisheidi", "Hydrothermal Fluid", "Middle Valley", "NGDS Content Model", "Nesjavellir", "REE", "Reykjanes", "Svartsengi", "USGIN Content Model", "aqueous chemistry", "geothermal", "mineral recovery", "rare earth element" ] |
| landingPage | https://gdr.openei.org/submissions/803 |
| license | https://creativecommons.org/licenses/by/4.0/ |
| modified | 2019-01-31T20:45:53Z |
| programCode |
[ "019:006" ] |
| projectLead | Arlene Anderson |
| projectNumber | EE0006748 |
| projectTitle | Maximizing Rare Earth Element Recovery in Geothermal Systems |
| publisher |
{ "name": "University of California", "@type": "org:Organization" } |
| spatial |
"{"type":"Polygon","coordinates":[[[-22.767681884766,63.780419237251],[-20.881266021729,63.780419237251],[-20.881266021729,64.289282821638],[-22.767681884766,64.289282821638],[-22.767681884766,63.780419237251]]]}"
|
| title | 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. |
