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Paleo-Pole Positions from Martian Magnetic Anomaly DataMagnetic component anomaly maps were made from five mapping cycles of the Mars Global Surveyor s magnetometer data. Our goal was to find and isolate positive and negative anomaly pairs which would indicate magnetization of a single source body. From these anomalies we could compute the direction of the magnetizing vector and subsequently the location of the magnetic pole existing at the time of magnetization. We found nine suitable anomaly pairs and from these we computed four North and 3 South poles with two at approximately 60 degrees north latitude. These results suggest that during the existence of the Martian main magnetic field it experienced several reversals.
Document ID
20030112411
Acquisition Source
Goddard Space Flight Center
Document Type
Preprint (Draft being sent to journal)
Authors
Taylor, Patrick T.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Frawley, James J.
(Herring Bay Geophysics, Inc. Tracys Landing, MD, United States)
Date Acquired
September 7, 2013
Publication Date
January 1, 2003
Subject Category
Geophysics
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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