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The behavior of the ancient geomagnetic field: How long has the geomagnetic field been essentially dipolar? Why does the magnetic field reverse? How strong can the magnetic field get? How fast can it change?
Statistical analysis of paleomagnetic data.
Applications of paleomagnetic data to geological problems such as: The use of paleomagnetic data for geochronological control. The use of paleointensity variations as an additional magnetostratigraphic tool.
Rock fabrics: The use of paleomagnetic data in structural and tectonic problems
The behavior of the ancient geomagnetic field: How long has the geomagnetic field been essentially dipolar? Why does the magnetic field reverse? How strong can the magnetic field get? How fast can it change?
Statistical analysis of paleomagnetic data.
Applications of paleomagnetic data to geological problems such as: The use of paleomagnetic data for geochronological control. The use of paleointensity variations as an additional magnetostratigraphic tool.
Rock fabrics: The use of paleomagnetic data in structural and tectonic problems
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PLOS ONEno. 1 (2024): e0293014-e0293014
Interdisciplinary contributions to archaeologypp.1753-1774, (2023)
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JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTHno. 8 (2023)
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTHno. 6 (2023)
Geochemistry, Geophysics, Geosystemsno. 6 (2023): n/a-n/a
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICAno. 52 (2023): e2313361120-e2313361120
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