Major element chemistry of the geothermal sea-water at Reykjanes and Svartsengi, Iceland
land represent localized anomalies of hot, altered rock in the uppermost part of the crust, which coincide with points of maximum tectonic/magmatic activity. These points correspond to the intersection of oblique fault swarms to the plate boundaries. Geothermal activity under mid-ocean ridges follow...
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| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.627.5014 http://www.minersoc.org/pages/Archive-MM/Volume_42/42-322-209.pdf |