Magnetic Anomaly data, Reykjanes Ridge, Langseth cruise MGL1309 (2013, investigators Fernando Martinez and Richard Hey)
This magnetic anomaly grid was derived from magnetic total field data acquired with a Geometrics G-882 Cesium magnetometer towed 200 m behind the ship. The International Geomagnetic Reference Field was removed from the total field values to produce the magnetic anomaly which was gridded in 0.5 minut...
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Online Access: | https://dx.doi.org/10.1594/ieda/324492 http://doi.iedadata.org/324492 |
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ftdatacite:10.1594/ieda/324492 2023-05-15T17:32:13+02:00 Magnetic Anomaly data, Reykjanes Ridge, Langseth cruise MGL1309 (2013, investigators Fernando Martinez and Richard Hey) Martinez, Fernando Hey, Richard 2018 application/x-netcdf https://dx.doi.org/10.1594/ieda/324492 http://doi.iedadata.org/324492 en eng Interdisciplinary Earth Data Alliance (IEDA) http://www.marine-geo.org/tools/search/entry.php?id=MGL1309 http://www.marine-geo.org/tools/search/entry.php?id=MGL1309 https://dx.doi.org/10.1016/j.epsl.2016.09.057 https://dx.doi.org/10.1594/ieda/324494 Creative Commons Attribution-NonCommercial-Share Alike 3.0 United States [CC BY-NC-SA 3.0] http://creativecommons.org/licenses/by-nc-sa/3.0/us CC-BY-NC-SA MagneticAnomalyIGRF dataset Dataset 2018 ftdatacite https://doi.org/10.1594/ieda/324492 https://doi.org/10.1016/j.epsl.2016.09.057 https://doi.org/10.1594/ieda/324494 2021-11-05T12:55:41Z This magnetic anomaly grid was derived from magnetic total field data acquired with a Geometrics G-882 Cesium magnetometer towed 200 m behind the ship. The International Geomagnetic Reference Field was removed from the total field values to produce the magnetic anomaly which was gridded in 0.5 minute cells using GMT-5 software (Wessel et al., 2013). The magnetic survey was conducted at the southern end of the Reykjanes Ridge, a segment of the Mid-Atlantic Ridge, in 2013 during Langseth cruise MGL1309 (investigators Fernando Martinez and Richard Hey). The data file is in netCDF:GMT grid format. It is cited in Martinez and Hey, 2017, and was generated as part of the project called Test Between Thermal and Tectonic Hypotheses for North Atlantic Seafloor Spreading Geometry Reorganization. Funding was provided by NSF award OCE11-54071. Dataset North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Mid-Atlantic Ridge Reykjanes ENVELOPE(-22.250,-22.250,65.467,65.467) Langseth ENVELOPE(15.668,15.668,68.338,68.338) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
MagneticAnomalyIGRF |
spellingShingle |
MagneticAnomalyIGRF Martinez, Fernando Hey, Richard Magnetic Anomaly data, Reykjanes Ridge, Langseth cruise MGL1309 (2013, investigators Fernando Martinez and Richard Hey) |
topic_facet |
MagneticAnomalyIGRF |
description |
This magnetic anomaly grid was derived from magnetic total field data acquired with a Geometrics G-882 Cesium magnetometer towed 200 m behind the ship. The International Geomagnetic Reference Field was removed from the total field values to produce the magnetic anomaly which was gridded in 0.5 minute cells using GMT-5 software (Wessel et al., 2013). The magnetic survey was conducted at the southern end of the Reykjanes Ridge, a segment of the Mid-Atlantic Ridge, in 2013 during Langseth cruise MGL1309 (investigators Fernando Martinez and Richard Hey). The data file is in netCDF:GMT grid format. It is cited in Martinez and Hey, 2017, and was generated as part of the project called Test Between Thermal and Tectonic Hypotheses for North Atlantic Seafloor Spreading Geometry Reorganization. Funding was provided by NSF award OCE11-54071. |
format |
Dataset |
author |
Martinez, Fernando Hey, Richard |
author_facet |
Martinez, Fernando Hey, Richard |
author_sort |
Martinez, Fernando |
title |
Magnetic Anomaly data, Reykjanes Ridge, Langseth cruise MGL1309 (2013, investigators Fernando Martinez and Richard Hey) |
title_short |
Magnetic Anomaly data, Reykjanes Ridge, Langseth cruise MGL1309 (2013, investigators Fernando Martinez and Richard Hey) |
title_full |
Magnetic Anomaly data, Reykjanes Ridge, Langseth cruise MGL1309 (2013, investigators Fernando Martinez and Richard Hey) |
title_fullStr |
Magnetic Anomaly data, Reykjanes Ridge, Langseth cruise MGL1309 (2013, investigators Fernando Martinez and Richard Hey) |
title_full_unstemmed |
Magnetic Anomaly data, Reykjanes Ridge, Langseth cruise MGL1309 (2013, investigators Fernando Martinez and Richard Hey) |
title_sort |
magnetic anomaly data, reykjanes ridge, langseth cruise mgl1309 (2013, investigators fernando martinez and richard hey) |
publisher |
Interdisciplinary Earth Data Alliance (IEDA) |
publishDate |
2018 |
url |
https://dx.doi.org/10.1594/ieda/324492 http://doi.iedadata.org/324492 |
long_lat |
ENVELOPE(-22.250,-22.250,65.467,65.467) ENVELOPE(15.668,15.668,68.338,68.338) |
geographic |
Mid-Atlantic Ridge Reykjanes Langseth |
geographic_facet |
Mid-Atlantic Ridge Reykjanes Langseth |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
http://www.marine-geo.org/tools/search/entry.php?id=MGL1309 http://www.marine-geo.org/tools/search/entry.php?id=MGL1309 https://dx.doi.org/10.1016/j.epsl.2016.09.057 https://dx.doi.org/10.1594/ieda/324494 |
op_rights |
Creative Commons Attribution-NonCommercial-Share Alike 3.0 United States [CC BY-NC-SA 3.0] http://creativecommons.org/licenses/by-nc-sa/3.0/us |
op_rightsnorm |
CC-BY-NC-SA |
op_doi |
https://doi.org/10.1594/ieda/324492 https://doi.org/10.1016/j.epsl.2016.09.057 https://doi.org/10.1594/ieda/324494 |
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1766130234421149696 |