Ferrovolcanism on metal worlds and the origin of pallasites
Ferrovolcanism on metal worlds and the origin of pallasites
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Publisher
London: Nature Publishing Group UK
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Language
English
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Publisher
London: Nature Publishing Group UK
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Contents
As differentiated planetesimals cool, their cores can solidify from the outside in
1
, as evidenced by palaeomagnetic measurements and cooling-rate estimates of iron meteorites
2
,
3
. The details of outside-in solidification and fate of residual core melt are poorly understood. For a core primarily composed of iron and nickel all...
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Full title
Ferrovolcanism on metal worlds and the origin of pallasites
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TN_cdi_proquest_journals_2377660937
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2377660937
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ISSN
2397-3366
E-ISSN
2397-3366
DOI
10.1038/s41550-019-0885-x
