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).
Citation Formats
University of California. (2015). 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. [data set]. Retrieved from https://dx.doi.org/10.15121/1261975.
Fowler, Andrew. 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.. United States: N.p., 01 May, 2015. Web. doi: 10.15121/1261975.
Fowler, Andrew. 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.. United States. https://dx.doi.org/10.15121/1261975
Fowler, Andrew. 2015. "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.". United States. https://dx.doi.org/10.15121/1261975. https://gdr.openei.org/submissions/803.
@div{oedi_3505, 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.}, author = {Fowler, Andrew.}, abstractNote = {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).}, doi = {10.15121/1261975}, url = {https://gdr.openei.org/submissions/803}, journal = {}, number = , volume = , place = {United States}, year = {2015}, month = {05}}
https://dx.doi.org/10.15121/1261975
Details
Data from May 1, 2015
Last updated Jan 31, 2019
Submitted Apr 27, 2016
Organization
University of California
Contact
Andrew Fowler
Authors
Original Source
https://gdr.openei.org/submissions/803Research Areas
Keywords
geothermal, Reykjanes, Svartsengi, Hellisheidi, Nesjavellir, Middle Valley, REE, Hydrothermal Fluid, Geothermal Fluid, rare earth element, mineral recovery, aqueous chemistry, AASG Geothermal Data, USGIN Content Model, NGDS Content ModelDOE Project Details
Project Name Maximizing Rare Earth Element Recovery in Geothermal Systems
Project Lead Arlene Anderson
Project Number EE0006748
