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 |
---|---|
Main Author: | |
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 |
id |
ftdoajarticles:oai:doaj.org/article:42628b48f4ae4d2989550eea5393234a |
---|---|
record_format |
openpolar |
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 |
_version_ |
1766287941259231232 |