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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Bibliographic Details
Published in:Annals of Geophysics
Main Author: Damaske, D.
Format: Article in Journal/Newspaper
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia, INGV 1999
Subjects:
Online Access:https://www.annalsofgeophysics.eu/index.php/annals/article/view/3710
https://doi.org/10.4401/ag-3710
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spelling 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
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