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...
Published in: | Annals of Geophysics |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Istituto Nazionale di Geofisica e Vulcanologia, INGV
1999
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Subjects: | |
Online Access: | https://www.annalsofgeophysics.eu/index.php/annals/article/view/3710 https://doi.org/10.4401/ag-3710 |
_version_ | 1821780646377291776 |
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author | Damaske, D. |
author_facet | Damaske, D. |
author_sort | Damaske, D. |
collection | Annals of Geophysics (INGV, Istituto Nazionale di Geofisica e Vulcanologia) |
container_issue | 2 |
container_title | Annals of Geophysics |
container_volume | 42 |
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 |
genre | antartic* Queen Maud Land |
genre_facet | antartic* Queen Maud Land |
geographic | Polar Plateau Queen Maud Land |
geographic_facet | Polar Plateau Queen Maud Land |
id | ftjaog:oai:ojs.annalsofgeophysics.eu:article/3710 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(0.000,0.000,-90.000,-90.000) ENVELOPE(12.000,12.000,-72.500,-72.500) |
op_collection_id | ftjaog |
op_doi | https://doi.org/10.4401/ag-3710 |
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_source | Annals of Geophysics; V. 42 N. 2 (1999) Annals of Geophysics; Vol. 42 No. 2 (1999) 2037-416X 1593-5213 |
publishDate | 1999 |
publisher | Istituto Nazionale di Geofisica e Vulcanologia, INGV |
record_format | openpolar |
spelling | ftjaog:oai:ojs.annalsofgeophysics.eu:article/3710 2025-01-16T19:45:30+00:00 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) Polar Plateau ENVELOPE(0.000,0.000,-90.000,-90.000) Queen Maud Land ENVELOPE(12.000,12.000,-72.500,-72.500) Annals of Geophysics 42 2 |
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 |
title | 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_short | Merging aeromagnetic data collected at different levels: the GEOMAUD survey |
title_sort | merging aeromagnetic data collected at different levels: the geomaud survey |
topic | Queen Maud Land Antartica aeromagnetics magnetic anomaly maps 04.05.99. General or miscellaneous |
topic_facet | Queen Maud Land Antartica aeromagnetics magnetic anomaly maps 04.05.99. General or miscellaneous |
url | https://www.annalsofgeophysics.eu/index.php/annals/article/view/3710 https://doi.org/10.4401/ag-3710 |