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

Journal of Geophysical Research: Planets

Volumn 101, Issue E6, 1996, Pages 14909-14932

  Kuramoto, Kiyoshi ^a,b   Matsui, Takafumi ^b  

^a TOKYO INSTITUTE OF TECHNOLOGY   (Japan)

^b UNIVERSITY OF TOKYO   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

ATMOSPHERIC EVOLUTION; CARBON; CORE; EARLY EARTH EVOLUTION; HYDROCARBON; MANTLE; PARTITIONING; REDOX; SILICATE MELT;

EID: 0030467770     PISSN: 01480227     EISSN: None     Source Type: Journal    
DOI: 10.1029/96JE00940     Document Type: Article

References (4)

1. Abe, Y., Abundance of carbon in an impact-induced proto atmosphere, in Proceedings of the 21st ISAS Lunar and Planetary Symposium, pp. 238-244. Inst. of Space and Astronaut. Sci., Sagamihara, Japan, 1988.
2. Abe, Y., Physical state of the very early Earth, Lithos, 30, 223-235, 1993.
3. Abe, Y., and T. Matsui, Early evolution of the Earth: Accretion, atmosphere formation, and thermal history, Proc. Lunar Planet. Sci. Conf. 17th, Part 1, J. Geophys. Res., 91, suppl., E291-E302, 1986.
4. Ahrens, T. J., Impact erosion of terrestrial planetary atmospheres, Annu. Rev. Earth Planet. Sci., 21, 525-555, 1993.