Climate-driven variations in geothermal activity in the northern Kenya rift valley
HIGH-TEMPERATURE continental geothermal systems are primarily associated with volcanic activity at plate margins 1 . It has long been known that the activity of these geothermal systems is intermittent, and this is generally attributed to the effect of magmatic intrusions or fault motions. Recently,...
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Veröffentlicht in: | Nature (London) 1993-03, Vol.362 (6417), p.233-234 |
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