FLUID ORIGIN AND DYNAMIC AT THE NEWLY DEVELOPED THEISTAREYKIR GEOTHERMAL FIELD, ICELAND
This study aim at deciphering the origin of the fluids and the hydrodynamic of the Theistareykir geothermal system using water isotopes and noble gases as a tracer of these respective contributions. Results first confirm that the magma beneath Theistareykir is a mix between a mantle plume (OIB) and...
| Main Authors: | , , , , , , , , |
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| Format: | Conference Object |
| Language: | unknown |
| Published: |
Zenodo
2019
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| Subjects: | |
| Online Access: | https://dx.doi.org/10.5281/zenodo.3566003 https://zenodo.org/record/3566003 |
| _version_ | 1821549563516813312 |
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| author | Saby, Marion Pinti, Daniele Hinsbger, Vincent Van Gautason, Bjarni Sigurðardóttir, Ásgerður Castro, Clara Hall, Chris Jean-François Hélie Rocher, Océane |
| author_facet | Saby, Marion Pinti, Daniele Hinsbger, Vincent Van Gautason, Bjarni Sigurðardóttir, Ásgerður Castro, Clara Hall, Chris Jean-François Hélie Rocher, Océane |
| author_sort | Saby, Marion |
| collection | DataCite |
| description | This study aim at deciphering the origin of the fluids and the hydrodynamic of the Theistareykir geothermal system using water isotopes and noble gases as a tracer of these respective contributions. Results first confirm that the magma beneath Theistareykir is a mix between a mantle plume (OIB) and an ocean ridge basalt (MORB). They also show that both magmatic fluids and surface water are present in the system in proportions that are being quantifyed. Water isotopes show that sources of surface water range from modern to Pre-Holocene. A crustal input is also present in the system with an enrichment in δ 18 O highlighting water-rock interaction. |
| format | Conference Object |
| genre | Iceland |
| genre_facet | Iceland |
| id | ftdatacite:10.5281/zenodo.3566003 |
| institution | Open Polar |
| language | unknown |
| op_collection_id | ftdatacite |
| op_doi | https://doi.org/10.5281/zenodo.3566003 https://doi.org/10.5281/zenodo.3566002 |
| op_relation | https://dx.doi.org/10.5281/zenodo.3566002 |
| op_rights | Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess |
| op_rightsnorm | CC-BY |
| publishDate | 2019 |
| publisher | Zenodo |
| record_format | openpolar |
| spelling | ftdatacite:10.5281/zenodo.3566003 2025-01-16T22:32:52+00:00 FLUID ORIGIN AND DYNAMIC AT THE NEWLY DEVELOPED THEISTAREYKIR GEOTHERMAL FIELD, ICELAND Saby, Marion Pinti, Daniele Hinsbger, Vincent Van Gautason, Bjarni Sigurðardóttir, Ásgerður Castro, Clara Hall, Chris Jean-François Hélie Rocher, Océane 2019 https://dx.doi.org/10.5281/zenodo.3566003 https://zenodo.org/record/3566003 unknown Zenodo https://dx.doi.org/10.5281/zenodo.3566002 Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess CC-BY Noble gas isotopes water isotopes geothermal field Theistareykir Iceland Text Conference paper article-journal ScholarlyArticle 2019 ftdatacite https://doi.org/10.5281/zenodo.3566003 https://doi.org/10.5281/zenodo.3566002 2021-11-05T12:55:41Z This study aim at deciphering the origin of the fluids and the hydrodynamic of the Theistareykir geothermal system using water isotopes and noble gases as a tracer of these respective contributions. Results first confirm that the magma beneath Theistareykir is a mix between a mantle plume (OIB) and an ocean ridge basalt (MORB). They also show that both magmatic fluids and surface water are present in the system in proportions that are being quantifyed. Water isotopes show that sources of surface water range from modern to Pre-Holocene. A crustal input is also present in the system with an enrichment in δ 18 O highlighting water-rock interaction. Conference Object Iceland DataCite |
| spellingShingle | Noble gas isotopes water isotopes geothermal field Theistareykir Iceland Saby, Marion Pinti, Daniele Hinsbger, Vincent Van Gautason, Bjarni Sigurðardóttir, Ásgerður Castro, Clara Hall, Chris Jean-François Hélie Rocher, Océane FLUID ORIGIN AND DYNAMIC AT THE NEWLY DEVELOPED THEISTAREYKIR GEOTHERMAL FIELD, ICELAND |
| title | FLUID ORIGIN AND DYNAMIC AT THE NEWLY DEVELOPED THEISTAREYKIR GEOTHERMAL FIELD, ICELAND |
| title_full | FLUID ORIGIN AND DYNAMIC AT THE NEWLY DEVELOPED THEISTAREYKIR GEOTHERMAL FIELD, ICELAND |
| title_fullStr | FLUID ORIGIN AND DYNAMIC AT THE NEWLY DEVELOPED THEISTAREYKIR GEOTHERMAL FIELD, ICELAND |
| title_full_unstemmed | FLUID ORIGIN AND DYNAMIC AT THE NEWLY DEVELOPED THEISTAREYKIR GEOTHERMAL FIELD, ICELAND |
| title_short | FLUID ORIGIN AND DYNAMIC AT THE NEWLY DEVELOPED THEISTAREYKIR GEOTHERMAL FIELD, ICELAND |
| title_sort | fluid origin and dynamic at the newly developed theistareykir geothermal field, iceland |
| topic | Noble gas isotopes water isotopes geothermal field Theistareykir Iceland |
| topic_facet | Noble gas isotopes water isotopes geothermal field Theistareykir Iceland |
| url | https://dx.doi.org/10.5281/zenodo.3566003 https://zenodo.org/record/3566003 |