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The hydrothermal system associated with the Kilauea East Rift Zone, Hawaii

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dc.contributor.author Thomas, Donald M.
dc.contributor.author Conrad, Mark E.
dc.date.accessioned 2020-04-21T00:00:06Z
dc.date.accessioned 2020-04-21T01:11:46Z
dc.date.available 2020-04-21T00:00:06Z
dc.date.available 2020-04-21T01:11:46Z
dc.date.issued 1997
dc.identifier.citation Thomas DM, Conrad ME. 1997. The hydrothermal system associated with the Kilauea East Rift Zone, Hawaii. IEEE.
dc.identifier.uri http://hdl.handle.net/10524/63229
dc.description.abstract During the last twenty years drilling and fluid production on the Kilauea East Rift Zone (KERZ), Hawaii, has shown that an active hydrothermal system is associated with much of the rift. Well logging and fluid geochemistry indicate that reservoir temperatures exceed 360/spl deg/C but are highly variable. Although neither well testing nor pressure decline data have clearly demonstrated the lateral limits of the reservoir, divergent fluid compositions over short distances suggest that the larger hydrothermal system is strongly compartmentalized across the rift zone. The chemical compositions of production fluids indicate that recharge is derived from ocean water and meteoric recharge and isotopic data suggest that the latter may be derived from subsurface inflow from the flanks of Mauna Loa.
dc.description.abstract Published in: IECEC-97 Proceedings of the Thirty-Second Intersociety Energy Conversion Engineering Conference (Cat. No.97CH6203)
dc.description.abstract Date of Conference: 27 July-1 Aug. 1997
dc.format.extent 6 pages
dc.language.iso eng
dc.publisher IEEE
dc.subject HGP-A
dc.subject hydrothermal
dc.subject chemistry
dc.subject Kilauea
dc.subject Big Island
dc.subject Hawaii
dc.subject.lcsh Geothermal resources--Hawaii--Hawaii Island
dc.subject.lcsh Geothermal resources--Hawaiʻi
dc.title The hydrothermal system associated with the Kilauea East Rift Zone, Hawaii
dc.type Journal Article
dc.type.dcmi Text
Appears in Collections: The Geothermal Collection


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