Crustal remanence and the magnetic moment of Mercury
作者： A. Stephenson
DOI: 10.1016/0012-821X(76)90206-5
关键词: Nuclear magnetic moment 、 Dipole 、 Geophysics 、 Condensed matter physics 、 Neutron magnetic moment 、 Magnetic dipole 、 Transition dipole moment 、 Electric dipole moment 、 Mercury's magnetic field 、 Electron magnetic dipole moment 、 Physics
摘要: Abstract The magnetic dipole moment of Mercury can be explained on the basis thermoremanent magnetization acquired by an outer shell in ancient Mercurian field produced internal source such as a core dynamo which is now inactive. Such will give rise to provided that there are differences permeability between and interior, or free space. By assuming properties surface rocks similar those Moon it shown fields order 1 gauss iron concentrations few percent sufficient produce present moment.
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