Oxide‐metal equilibria to 2500°C and 25 GPa: Implications for core formation and the light component in the Earth's core

Publisher： John Wiley & Sons Inc

E-ISSN： 2156-2202|103|B6|12239-12260

ISSN： 0148-0227

Source： Journal Of Geophysical Research, Vol.103, Iss.B6, 1998-06, pp. : 12239-12260

Disclaimer: Any content in publications that violate the sovereignty, the constitution or regulations of the PRC is not accepted or approved by CNPIEC.

Previous Menu Next

Related content

Partitioning of H and C between the mantle and core during the core formation in the Earth: Its implications for the atmospheric evolution and redox state of early mantle

By  

Journal Of Geophysical Research, Vol. 101, Iss. E6, 1996-06 ,pp. : 14909-14932

John Wiley & Sons Inc

Access to resources Recommend Favorite

An equation of state for liquid iron and implications for the Earth's core

By  

Journal Of Geophysical Research, Vol. 99, Iss. B3, 1994-03 ,pp. : 4273-4284

John Wiley & Sons Inc

Access to resources Recommend Favorite

Core formation in the shergottite parent body and comparison with the Earth

By  

Journal Of Geophysical Research, Vol. 92, Iss. B4, 1987-03 ,pp. : E627-E632

John Wiley & Sons Inc

Access to resources Recommend Favorite

Thermal equation of state of Fe3S and implications for sulfur in Earth's core

By  

Journal Of Geophysical Research, Vol. 111, Iss. B6, 2006-06 ,pp. : n/a-n/a

John Wiley & Sons Inc

Access to resources Recommend Favorite

Static compression of iron‐silicon alloys: Implications for silicon in the Earth's core

By  

Journal Of Geophysical Research, Vol. 108, Iss. B1, 2003-01 ,pp. : n/a-n/a

John Wiley & Sons Inc

Access to resources Recommend Favorite