Published August 21, 1975
| public
Journal Article
Dynamo generation in Mercury
- Creators
-
Stevenson, D. J.
Chicago
Abstract
Observations during the most recent encounter of the planet Mercury by Mariner 10 seem to have confirmed the existence of a small but intrinsic magnetic dipole of about 3 × 10^(−3) gauss R_M^3, where R_M is the radius of Mercury. This field may be small enough to have a non-dynamo explanation, but it is nevertheless of interest to examine whether dynamo generation is possible for the present Mercury.
Additional Information
© 1975 Nature Publishing Group. Received June 9; accepted July 1, 1975. I thank F. H. Busse, N. F. Ness, and S. C. Solomon for discussions. This work is supported by grants from NASA and the NSF.Additional details
- Eprint ID
- 38902
- Resolver ID
- CaltechAUTHORS:20130612-084611913
- NASA
- NSF
- Created
-
2013-06-12Created from EPrint's datestamp field
- Updated
-
2021-11-09Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences (GPS)