Results Of Televiewer Logging In Well K-18 In Krafla High Temperature Area, Ne-Iceland
Televiewer logging was performed in well K-18 in Krafla high temperature field at 470 – 2180 m depth in October 2014 as a part of the IMAGE (Integrated Methods for Advanced Geothermal Exploration) European project. Results of structural analysis on grounds of the Televiewer data indicate that joints...
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ftdatacite:10.5281/zenodo.1291140 2023-05-15T16:47:35+02:00 Results Of Televiewer Logging In Well K-18 In Krafla High Temperature Area, Ne-Iceland Árnadóttir, Sigurveig 2018 https://dx.doi.org/10.5281/zenodo.1291140 https://zenodo.org/record/1291140 en eng Zenodo https://dx.doi.org/10.5281/zenodo.1291141 Open Access info:eu-repo/semantics/openAccess geothermal energy exploration geophysics krafla televiewer logging well K-18 high temperature area iceland Text Report report ScholarlyArticle 2018 ftdatacite https://doi.org/10.5281/zenodo.1291140 https://doi.org/10.5281/zenodo.1291141 2021-11-05T12:55:41Z Televiewer logging was performed in well K-18 in Krafla high temperature field at 470 – 2180 m depth in October 2014 as a part of the IMAGE (Integrated Methods for Advanced Geothermal Exploration) European project. Results of structural analysis on grounds of the Televiewer data indicate that joints and fractures within the logged interval predominantly strike from NW-SE to N-S and dip towards NE/E. Fractures and joints observed in the Televiewer images are filled/cemented or tight/discontinuous, and in several cases partially open. No major open fractures were observed within the logged interval. Interfaces observed in the Televiewer images are considered to mark intrusion boundaries, and can be roughly divided into steeply dipping N-S and NE-SW striking interfaces (dykes) and sub-horizontal ~WNW-ESE striking, ~SSW-dipping interfaces (sill intrusions). The latter are in some cases non planar, which may suggest that magma intruded a still unsolidified intrusive material. Report Iceland DataCite Metadata Store (German National Library of Science and Technology) Krafla ENVELOPE(-16.747,-16.747,65.713,65.713) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
geothermal energy exploration geophysics krafla televiewer logging well K-18 high temperature area iceland |
spellingShingle |
geothermal energy exploration geophysics krafla televiewer logging well K-18 high temperature area iceland Árnadóttir, Sigurveig Results Of Televiewer Logging In Well K-18 In Krafla High Temperature Area, Ne-Iceland |
topic_facet |
geothermal energy exploration geophysics krafla televiewer logging well K-18 high temperature area iceland |
description |
Televiewer logging was performed in well K-18 in Krafla high temperature field at 470 – 2180 m depth in October 2014 as a part of the IMAGE (Integrated Methods for Advanced Geothermal Exploration) European project. Results of structural analysis on grounds of the Televiewer data indicate that joints and fractures within the logged interval predominantly strike from NW-SE to N-S and dip towards NE/E. Fractures and joints observed in the Televiewer images are filled/cemented or tight/discontinuous, and in several cases partially open. No major open fractures were observed within the logged interval. Interfaces observed in the Televiewer images are considered to mark intrusion boundaries, and can be roughly divided into steeply dipping N-S and NE-SW striking interfaces (dykes) and sub-horizontal ~WNW-ESE striking, ~SSW-dipping interfaces (sill intrusions). The latter are in some cases non planar, which may suggest that magma intruded a still unsolidified intrusive material. |
format |
Report |
author |
Árnadóttir, Sigurveig |
author_facet |
Árnadóttir, Sigurveig |
author_sort |
Árnadóttir, Sigurveig |
title |
Results Of Televiewer Logging In Well K-18 In Krafla High Temperature Area, Ne-Iceland |
title_short |
Results Of Televiewer Logging In Well K-18 In Krafla High Temperature Area, Ne-Iceland |
title_full |
Results Of Televiewer Logging In Well K-18 In Krafla High Temperature Area, Ne-Iceland |
title_fullStr |
Results Of Televiewer Logging In Well K-18 In Krafla High Temperature Area, Ne-Iceland |
title_full_unstemmed |
Results Of Televiewer Logging In Well K-18 In Krafla High Temperature Area, Ne-Iceland |
title_sort |
results of televiewer logging in well k-18 in krafla high temperature area, ne-iceland |
publisher |
Zenodo |
publishDate |
2018 |
url |
https://dx.doi.org/10.5281/zenodo.1291140 https://zenodo.org/record/1291140 |
long_lat |
ENVELOPE(-16.747,-16.747,65.713,65.713) |
geographic |
Krafla |
geographic_facet |
Krafla |
genre |
Iceland |
genre_facet |
Iceland |
op_relation |
https://dx.doi.org/10.5281/zenodo.1291141 |
op_rights |
Open Access info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5281/zenodo.1291140 https://doi.org/10.5281/zenodo.1291141 |
_version_ |
1766037682686787584 |