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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ftciteseerx:oai:CiteSeerX.psu:10.1.1.627.5014 2023-05-15T16:46:48+02:00 Major element chemistry of the geothermal sea-water at Reykjanes and Svartsengi, Iceland Stefan Arnorsson The Pennsylvania State University CiteSeerX Archives application/pdf 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 en eng 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 Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.minersoc.org/pages/Archive-MM/Volume_42/42-322-209.pdf text ftciteseerx 2016-01-08T15:17:28Z 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 follows probably similar tectonic/magmatic nomalies. Due to high permeability sea-water invades the bed-rock of the Reykjanes Peninsula, Iceland, and is overlain by a variably thick lens of dilute ground water ofmeteoric origin. The variable degree of salinity of geothermal waters in the Reykjanes Peninsula has resulted from different degree of mixing of fresh ground water with the underlying sea-water-ground-water in the downflow zones around the geothermal fields. At Reykjanes the Text Iceland Unknown Reykjanes ENVELOPE(-22.250,-22.250,65.467,65.467) |
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ftciteseerx |
language |
English |
description |
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 follows probably similar tectonic/magmatic nomalies. Due to high permeability sea-water invades the bed-rock of the Reykjanes Peninsula, Iceland, and is overlain by a variably thick lens of dilute ground water ofmeteoric origin. The variable degree of salinity of geothermal waters in the Reykjanes Peninsula has resulted from different degree of mixing of fresh ground water with the underlying sea-water-ground-water in the downflow zones around the geothermal fields. At Reykjanes the |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Stefan Arnorsson |
spellingShingle |
Stefan Arnorsson Major element chemistry of the geothermal sea-water at Reykjanes and Svartsengi, Iceland |
author_facet |
Stefan Arnorsson |
author_sort |
Stefan Arnorsson |
title |
Major element chemistry of the geothermal sea-water at Reykjanes and Svartsengi, Iceland |
title_short |
Major element chemistry of the geothermal sea-water at Reykjanes and Svartsengi, Iceland |
title_full |
Major element chemistry of the geothermal sea-water at Reykjanes and Svartsengi, Iceland |
title_fullStr |
Major element chemistry of the geothermal sea-water at Reykjanes and Svartsengi, Iceland |
title_full_unstemmed |
Major element chemistry of the geothermal sea-water at Reykjanes and Svartsengi, Iceland |
title_sort |
major element chemistry of the geothermal sea-water at reykjanes and svartsengi, iceland |
url |
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 |
long_lat |
ENVELOPE(-22.250,-22.250,65.467,65.467) |
geographic |
Reykjanes |
geographic_facet |
Reykjanes |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
http://www.minersoc.org/pages/Archive-MM/Volume_42/42-322-209.pdf |
op_relation |
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 |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766036902974062592 |