Why no anomaly is visible over most of the continent-ocean boundary in the global crustal magnetic field

Physics of the Earth and Planetary Interiors

Volumn 149, Issue 3-4, 2005, Pages 321-333

  Hemant, Kumar ^a   Maus, Stefan ^b,c  

^a GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

^b UNIVERSITY OF COLORADO   (United States)

^c NATIONAL GEOPHYSICAL DATA CENTER   (United States)

Author keywords

Continent ocean anomaly; Global; Vertically integrated susceptibility (VIS)

Indexed keywords

CRYSTALS; GEOGRAPHIC INFORMATION SYSTEMS; MAGNETIC PROPERTIES; MAGNETIZATION; MAPS; MATHEMATICAL MODELS; ROCKS; SATELLITES;

ANOMALY; CONTINENT-OCEAN BOUNDARY; MAGNETIC ANOMALY MAPS; MAGNETIZATION MODELS;

GEOLOGY;

ANOMALY; GEOMAGNETIC FIELD; GIS; MAGNETIC SUSCEPTIBILITY; OCEAN-CONTINENT TRANSITION;

EID: 14944382713     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2004.10.007     Document Type: Article

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