Format:
Online-Ressource
ISSN:
1617-4011
Content:
Abstract γ Fe γ Fe W FePt fcc = - 121.5 ± 2.1 kJ mol- 1 W PtFe fcc = - 93.3 ± 4.3 kJ mol- 1 W FePt liq = - 124.5 kJ mol- 1 W PtFe liq = - 94.0 kJ mol- 1 a Fe a FeO f O 2 under conditions relevant to magma oceans, core formation, and differentiation processes in the lower mantle of Earth or on other terrestrial planets. Improvements in these models require new constraints on the equation of state of FePt fcc alloy and documentation of the high-pressure melting relations in the system Fe–Pt.
In:
volume:35
In:
number:5
In:
year:2023
In:
pages:789-803
In:
extent:15
In:
European journal of mineralogy, Göttingen : Copernicus Publications, 1989-, 35, Heft 5 (2023), 789-803 (gesamt 15), 1617-4011
Language:
English
DOI:
10.5194/ejm-35-789-2023
URN:
urn:nbn:de:101:1-2023092804324892844773
URL:
https://doi.org/10.5194/ejm-35-789-2023
URL:
https://nbn-resolving.org/urn:nbn:de:101:1-2023092804324892844773
URL:
https://d-nb.info/1304227863/34
URL:
https://ejm.copernicus.org/articles/35/789/2023/ejm-35-789-2023.pdf
URL:
https://ejm.copernicus.org/articles/35/789/2023/