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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Published in:Annals of Geophysics
Main Author: D. Damaske
Format: Article in Journal/Newspaper
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1999
Subjects:
Online Access:https://doi.org/10.4401/ag-3710
https://doaj.org/article/42628b48f4ae4d2989550eea5393234a
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spelling ftdoajarticles:oai:doaj.org/article:42628b48f4ae4d2989550eea5393234a 2023-05-15T14:15:36+02:00 Merging aeromagnetic data collected at different levels: the GEOMAUD survey D. Damaske 1999-06-01T00:00:00Z https://doi.org/10.4401/ag-3710 https://doaj.org/article/42628b48f4ae4d2989550eea5393234a EN eng Istituto Nazionale di Geofisica e Vulcanologia (INGV) http://www.annalsofgeophysics.eu/index.php/annals/article/view/3710 https://doaj.org/toc/1593-5213 https://doaj.org/toc/2037-416X doi:10.4401/ag-3710 1593-5213 2037-416X https://doaj.org/article/42628b48f4ae4d2989550eea5393234a Annals of Geophysics, Vol 42, Iss 2 (1999) Queen Maud Land Antartica aeromagnetics magnetic anomaly maps Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 article 1999 ftdoajarticles https://doi.org/10.4401/ag-3710 2022-12-31T04:23:21Z 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 Directory of Open Access Journals: DOAJ Articles 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 Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Queen Maud Land
Antartica
aeromagnetics
magnetic anomaly maps
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
spellingShingle Queen Maud Land
Antartica
aeromagnetics
magnetic anomaly maps
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
D. Damaske
Merging aeromagnetic data collected at different levels: the GEOMAUD survey
topic_facet Queen Maud Land
Antartica
aeromagnetics
magnetic anomaly maps
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
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 D. Damaske
author_facet D. Damaske
author_sort D. Damaske
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://doi.org/10.4401/ag-3710
https://doaj.org/article/42628b48f4ae4d2989550eea5393234a
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, Vol 42, Iss 2 (1999)
op_relation http://www.annalsofgeophysics.eu/index.php/annals/article/view/3710
https://doaj.org/toc/1593-5213
https://doaj.org/toc/2037-416X
doi:10.4401/ag-3710
1593-5213
2037-416X
https://doaj.org/article/42628b48f4ae4d2989550eea5393234a
op_doi https://doi.org/10.4401/ag-3710
container_title Annals of Geophysics
container_volume 42
container_issue 2
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