Compound and Elemental Analysis At Geysers Area (Kennedy & Truesdell, 1996)

From Open Energy Information

Exploration Activity: Compound and Elemental Analysis At Geysers Area (Kennedy & Truesdell, 1996)

Exploration Activity Details
Location Geysers Area
Exploration Technique Compound and Elemental Analysis
Activity Date
Usefulness could be useful with more improvements
DOE-funding Unknown

 
Notes
The evidence provided by the noble gases for a magmatic gas component in the Northwest Geysers adds new constraints to genetic models of the system and its evolution. The high proportion of magmatic gas and high total NCG in HTR steam are inconsistent with an origin of the vapor-dominated Northwest Geysers reservoir from deep boiling of a connate or metamorphic water. Instead, the strong magmatic component suggests that the HTR and the sharp HTR/NTR boundary observed in the Northwest Geysers reservoir were formed and are sustained by an active flux of magmatic volatiles.


Additional References


<metadesc> Compound and Elemental Analysis At Geysers Area (Kennedy & Truesdell, 1996): geothermal exploration activity. </metadesc>