Terrestrial Accretion Under Oxidizing Conditions
Terrestrial Accretion Under Oxidizing Conditions
About this item
Full title
Author / Creator
Publisher
United States: American Association for the Advancement of Science
Journal title
Language
English
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Publisher
United States: American Association for the Advancement of Science
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Scope and Contents
Contents
The abundance of siderophile elements in the mantle preserves the signature of core formation. On the basis of partitioning experiments at high pressure (35 to 74 gigapascals) and high temperature (3100 to 4400 kelvin), we demonstrate that depletions of slightly siderophile elements (vanadium and chromium), as well as moderately siderophile element...
Alternative Titles
Full title
Terrestrial Accretion Under Oxidizing Conditions
Authors, Artists and Contributors
Author / Creator
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Record Identifier
TN_cdi_hal_primary_oai_HAL_hal_00799054v1
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_00799054v1
Other Identifiers
ISSN
0036-8075
E-ISSN
1095-9203
DOI
10.1126/science.1227923
