Difference between revisions of "Isotopic Analysis At Yellowstone Region (Sturchio, Et Al., 1990)"

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(Created page with "{{ExplorationActivity |Name=Isotopic Analysis At Yellowstone Region (Sturchio, Et Al., 1990) |Technique=Isotopic Analysis |Place=Yellowstone Caldera Geothermal Region |Notes=Ther...")
 
 
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{{ExplorationActivity
 
{{ExplorationActivity
|Name=Isotopic Analysis At Yellowstone Region (Sturchio, Et Al., 1990)
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|Name=Isotopic Analysis- Fluid At Yellowstone Region (Sturchio, Et Al., 1990)
|Technique=Isotopic Analysis
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|Technique=Isotopic Analysis- Fluid
 
|Place=Yellowstone Caldera Geothermal Region
 
|Place=Yellowstone Caldera Geothermal Region
 
|Notes=There are two possible explanations for the inferred presence of relatively 18O-enriched thermal water at Yellowstone in the past: (1) meteoric recharge water was relatively lSO-enriched at certain times because of temporal variations in climate, or (2) meteoric recharge water was not relatively iaO-enriched, but rather thermal water was enriched in iaO by hydrothermal processes.
 
|Notes=There are two possible explanations for the inferred presence of relatively 18O-enriched thermal water at Yellowstone in the past: (1) meteoric recharge water was relatively lSO-enriched at certain times because of temporal variations in climate, or (2) meteoric recharge water was not relatively iaO-enriched, but rather thermal water was enriched in iaO by hydrothermal processes.

Latest revision as of 11:30, 7 October 2013

Exploration Activity: Isotopic Analysis At Yellowstone Region (Sturchio, Et Al., 1990)

Exploration Activity Details
Location Yellowstone Caldera Geothermal Region
Exploration Technique Isotopic Analysis- Fluid
Activity Date
Usefulness could be useful with more improvements
DOE-funding Unknown

 
Notes
There are two possible explanations for the inferred presence of relatively 18O-enriched thermal water at Yellowstone in the past: (1) meteoric recharge water was relatively lSO-enriched at certain times because of temporal variations in climate, or (2) meteoric recharge water was not relatively iaO-enriched, but rather thermal water was enriched in iaO by hydrothermal processes.

 
References


Additional References