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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.

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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.
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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

Andrew Fowler

University of California

Research Areas

DOE Project Details

Project Name Maximizing Rare Earth Element Recovery in Geothermal Systems

Project Lead Arlene Anderson

Project Number EE0006748

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