Mapping and interpretation of satellite magnetic anomalies from POGO data over the Antarctic region

A satellite magnetic anomaly map made using the POGO magnetic field data is compared to three maps made using Magsat data. A total of 14 anomalies with magnitudes greater than 3 nT can be identified in all four of the maps poleward of 60°S latitude. Forward models of the Antarctic continental and oc...

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Published in:Annals of Geophysics
Main Authors: Purucker, M. E., von Frese, R. R. B., Taylor, P. T.
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/3715
https://doi.org/10.4401/ag-3715
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spelling ftjaog:oai:ojs.annalsofgeophysics.eu:article/3715 2023-05-15T13:54:52+02:00 Mapping and interpretation of satellite magnetic anomalies from POGO data over the Antarctic region Purucker, M. E. von Frese, R. R. B. Taylor, P. T. 1999-11-25 application/pdf https://www.annalsofgeophysics.eu/index.php/annals/article/view/3715 https://doi.org/10.4401/ag-3715 eng eng Istituto Nazionale di Geofisica e Vulcanologia, INGV https://www.annalsofgeophysics.eu/index.php/annals/article/view/3715/3779 https://www.annalsofgeophysics.eu/index.php/annals/article/view/3715 doi:10.4401/ag-3715 Annals of Geophysics; V. 42 N. 2 (1999) Annals of Geophysics; Vol. 42 No. 2 (1999) 2037-416X 1593-5213 Antarctic geomagnetic field magnetic field satellites magnetic anomalies 04.05.04. Magnetic anomalies info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1999 ftjaog https://doi.org/10.4401/ag-3715 2022-03-27T06:36:31Z A satellite magnetic anomaly map made using the POGO magnetic field data is compared to three maps made using Magsat data. A total of 14 anomalies with magnitudes greater than 3 nT can be identified in all four of the maps poleward of 60°S latitude. Forward models of the Antarctic continental and oceanic lithosphere are produced which use magnetic crustal thickness based on seismic and heat flow data, and which also use the distribution of the Cretaceous Quiet Zone from marine geophysics. These simple models can explain significant parts of eight of the 14 identified anomalies. The remaining anomalies may be caused by lateral variations of magnetization, inadequate models of the magnetic crustal thickness, or remanent magnetizations in directions other than the present field. In addition, contamination of the magnetic anomaly maps by fields of time-varying external origin (and their corresponding internal parts) is still a significant problem in the Antarctic region. Article in Journal/Newspaper Antarc* Antarctic Annals of Geophysics (INGV, Istituto Nazionale di Geofisica e Vulcanologia) Antarctic The Antarctic 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 Antarctic
geomagnetic field
magnetic field satellites
magnetic anomalies
04.05.04. Magnetic anomalies
spellingShingle Antarctic
geomagnetic field
magnetic field satellites
magnetic anomalies
04.05.04. Magnetic anomalies
Purucker, M. E.
von Frese, R. R. B.
Taylor, P. T.
Mapping and interpretation of satellite magnetic anomalies from POGO data over the Antarctic region
topic_facet Antarctic
geomagnetic field
magnetic field satellites
magnetic anomalies
04.05.04. Magnetic anomalies
description A satellite magnetic anomaly map made using the POGO magnetic field data is compared to three maps made using Magsat data. A total of 14 anomalies with magnitudes greater than 3 nT can be identified in all four of the maps poleward of 60°S latitude. Forward models of the Antarctic continental and oceanic lithosphere are produced which use magnetic crustal thickness based on seismic and heat flow data, and which also use the distribution of the Cretaceous Quiet Zone from marine geophysics. These simple models can explain significant parts of eight of the 14 identified anomalies. The remaining anomalies may be caused by lateral variations of magnetization, inadequate models of the magnetic crustal thickness, or remanent magnetizations in directions other than the present field. In addition, contamination of the magnetic anomaly maps by fields of time-varying external origin (and their corresponding internal parts) is still a significant problem in the Antarctic region.
format Article in Journal/Newspaper
author Purucker, M. E.
von Frese, R. R. B.
Taylor, P. T.
author_facet Purucker, M. E.
von Frese, R. R. B.
Taylor, P. T.
author_sort Purucker, M. E.
title Mapping and interpretation of satellite magnetic anomalies from POGO data over the Antarctic region
title_short Mapping and interpretation of satellite magnetic anomalies from POGO data over the Antarctic region
title_full Mapping and interpretation of satellite magnetic anomalies from POGO data over the Antarctic region
title_fullStr Mapping and interpretation of satellite magnetic anomalies from POGO data over the Antarctic region
title_full_unstemmed Mapping and interpretation of satellite magnetic anomalies from POGO data over the Antarctic region
title_sort mapping and interpretation of satellite magnetic anomalies from pogo data over the antarctic region
publisher Istituto Nazionale di Geofisica e Vulcanologia, INGV
publishDate 1999
url https://www.annalsofgeophysics.eu/index.php/annals/article/view/3715
https://doi.org/10.4401/ag-3715
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
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/3715/3779
https://www.annalsofgeophysics.eu/index.php/annals/article/view/3715
doi:10.4401/ag-3715
op_doi https://doi.org/10.4401/ag-3715
container_title Annals of Geophysics
container_volume 42
container_issue 2
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