Merging aeromagnetic data collected at different levels: the GEOMAUD survey
As part of the German GEOMAUD-expedition an aeromagnetic survey was carried out in Central Queen Maud Land. The helicopter-borne survey was designed in a conventional form of a regional survey with a spacing of profile-lines of 4.4 km. Due to terrain considerations - surveying from the coast across...
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Istituto Nazionale di Geofisica e Vulcanologia, INGV
1999
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Online Access: | https://www.annalsofgeophysics.eu/index.php/annals/article/view/3710 https://doi.org/10.4401/ag-3710 |
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ftjaog:oai:ojs.annalsofgeophysics.eu:article/3710 2023-05-15T14:15:40+02:00 Merging aeromagnetic data collected at different levels: the GEOMAUD survey Damaske, D. 1999-11-25 application/pdf https://www.annalsofgeophysics.eu/index.php/annals/article/view/3710 https://doi.org/10.4401/ag-3710 eng eng Istituto Nazionale di Geofisica e Vulcanologia, INGV https://www.annalsofgeophysics.eu/index.php/annals/article/view/3710/3774 https://www.annalsofgeophysics.eu/index.php/annals/article/view/3710 doi:10.4401/ag-3710 Annals of Geophysics; V. 42 N. 2 (1999) Annals of Geophysics; Vol. 42 No. 2 (1999) 2037-416X 1593-5213 Queen Maud Land Antartica aeromagnetics magnetic anomaly maps 04.05.99. General or miscellaneous info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1999 ftjaog https://doi.org/10.4401/ag-3710 2022-03-27T06:36:31Z As part of the German GEOMAUD-expedition an aeromagnetic survey was carried out in Central Queen Maud Land. The helicopter-borne survey was designed in a conventional form of a regional survey with a spacing of profile-lines of 4.4 km. Due to terrain considerations - surveying from the coast across the mountain ranges to the high altitudes of the polar plateau - the survey was split into two sections flown at different constant levels. Over the coastal part survey elevation was 570 m (above sea level) while for the mountain section 2845 m was chosen. Both survey parts were processed separately. The low level section was upward continued before merging with the high level section. Though this leads to a homogeneous magnetic anomaly map, in some applications it may be more advantageous to present the anomalies of the magnetic field in original survey levels as a simple combined map because small scale features are preserved and can be used in recognizing magnetic units and patterns for geological/geophysical interpretation. Article in Journal/Newspaper antartic* Queen Maud Land Annals of Geophysics (INGV, Istituto Nazionale di Geofisica e Vulcanologia) Queen Maud Land ENVELOPE(12.000,12.000,-72.500,-72.500) Polar Plateau ENVELOPE(0.000,0.000,-90.000,-90.000) Annals of Geophysics 42 2 |
institution |
Open Polar |
collection |
Annals of Geophysics (INGV, Istituto Nazionale di Geofisica e Vulcanologia) |
op_collection_id |
ftjaog |
language |
English |
topic |
Queen Maud Land Antartica aeromagnetics magnetic anomaly maps 04.05.99. General or miscellaneous |
spellingShingle |
Queen Maud Land Antartica aeromagnetics magnetic anomaly maps 04.05.99. General or miscellaneous Damaske, D. Merging aeromagnetic data collected at different levels: the GEOMAUD survey |
topic_facet |
Queen Maud Land Antartica aeromagnetics magnetic anomaly maps 04.05.99. General or miscellaneous |
description |
As part of the German GEOMAUD-expedition an aeromagnetic survey was carried out in Central Queen Maud Land. The helicopter-borne survey was designed in a conventional form of a regional survey with a spacing of profile-lines of 4.4 km. Due to terrain considerations - surveying from the coast across the mountain ranges to the high altitudes of the polar plateau - the survey was split into two sections flown at different constant levels. Over the coastal part survey elevation was 570 m (above sea level) while for the mountain section 2845 m was chosen. Both survey parts were processed separately. The low level section was upward continued before merging with the high level section. Though this leads to a homogeneous magnetic anomaly map, in some applications it may be more advantageous to present the anomalies of the magnetic field in original survey levels as a simple combined map because small scale features are preserved and can be used in recognizing magnetic units and patterns for geological/geophysical interpretation. |
format |
Article in Journal/Newspaper |
author |
Damaske, D. |
author_facet |
Damaske, D. |
author_sort |
Damaske, D. |
title |
Merging aeromagnetic data collected at different levels: the GEOMAUD survey |
title_short |
Merging aeromagnetic data collected at different levels: the GEOMAUD survey |
title_full |
Merging aeromagnetic data collected at different levels: the GEOMAUD survey |
title_fullStr |
Merging aeromagnetic data collected at different levels: the GEOMAUD survey |
title_full_unstemmed |
Merging aeromagnetic data collected at different levels: the GEOMAUD survey |
title_sort |
merging aeromagnetic data collected at different levels: the geomaud survey |
publisher |
Istituto Nazionale di Geofisica e Vulcanologia, INGV |
publishDate |
1999 |
url |
https://www.annalsofgeophysics.eu/index.php/annals/article/view/3710 https://doi.org/10.4401/ag-3710 |
long_lat |
ENVELOPE(12.000,12.000,-72.500,-72.500) ENVELOPE(0.000,0.000,-90.000,-90.000) |
geographic |
Queen Maud Land Polar Plateau |
geographic_facet |
Queen Maud Land Polar Plateau |
genre |
antartic* Queen Maud Land |
genre_facet |
antartic* Queen Maud Land |
op_source |
Annals of Geophysics; V. 42 N. 2 (1999) Annals of Geophysics; Vol. 42 No. 2 (1999) 2037-416X 1593-5213 |
op_relation |
https://www.annalsofgeophysics.eu/index.php/annals/article/view/3710/3774 https://www.annalsofgeophysics.eu/index.php/annals/article/view/3710 doi:10.4401/ag-3710 |
op_doi |
https://doi.org/10.4401/ag-3710 |
container_title |
Annals of Geophysics |
container_volume |
42 |
container_issue |
2 |
_version_ |
1766287981258211328 |