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Stalking the magma ocean

Stevenson, David J. (1992) Stalking the magma ocean. Nature, 355 . p. 301. ISSN 0028-0836. https://resolver.caltech.edu/CaltechAUTHORS:20130702-095943237

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Abstract

Planets and smaller bodies are evidently differentiated, at least into a metallic core, silicate mantel and buoyant crust. Much of the differentiation occurred or began when the body was much hotter than now, back at the time of planetary formation around 4.5 thousand million years ago.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1038/355301a0DOIArticle
http://www.nature.com/nature/journal/v355/n6358/abs/355301a0.htmlPublisherArticle
ORCID:
AuthorORCID
Stevenson, David J.0000-0001-9432-7159
Additional Information:© 1992 Nature Publishing Group.
Record Number:CaltechAUTHORS:20130702-095943237
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20130702-095943237
Official Citation:Stevenson, D. J. (1992). "Stalking the magma ocean." Nature 355(6358): 301-301.
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:39182
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:02 Jul 2013 23:42
Last Modified:03 Oct 2019 05:04

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