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The Martian dynamo

โœ Scribed by Alexander Ruzmaikin


Book ID
116044982
Publisher
Elsevier Science
Year
1991
Tongue
English
Weight
560 KB
Volume
67
Category
Article
ISSN
0031-9201

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During late-stage planet formation, giant impacts produce localized mantle melt regions within which impactor iron droplets settle to the bottom near a permeability horizon. After accumulation, iron heated by the impact migrates downward to the core through colder, mostly solid mantle. The degree of