论文信息 - Cubanite: A New Sulfide Phase in CI Meteorites

Cubanite: A New Sulfide Phase in CI Meteorites

Cubanite (CuFe2S3), previously unobserved in meteorites, has been discovered in two carbonaceous chondrites, Orgueil and Alais. The association of this mineral with low-copper pyrrhotite suggests that it formed in a low-temperature environment on the meteorite parent body.

J. Kerridge | J. D. MacDougall | J. MacDougall

[1] J. Macdougall,et al. Mafic silicates in the Orgueil carbonaceous meteorite , 1976 .

[2] J. Kerridge. Major element composition of phyllosilicates in the Orgueil carbonaceous meteorite , 1976 .

[3] John S. Lewis,et al. Low temperature condensation from the solar nebula , 1972 .

[4] E. Anders,et al. CHEMICAL FRACTIONATIONS IN METEORITES. II. ABUNDANCE PATTERNS AND THEIR INTERPRETATION. , 1967 .

[5] John A. Wood,et al. A chemical-petrologic classification for the chondritic meteorites. , 1967 .

[6] G. Kullerud,et al. Thermal Stability of Assemblages in the Cu—Fe—S System , 1966 .

[7] J. Kerridge. LOW‐TEMPERATURE MINERALS FROM THE FINE‐GRAINED MATRIX OF SOME CARBONACEOUS METEORITES , 1964 .

[8] W. Meinschein,et al. AQUEOUS, LOW TEMPERATURE ENVIRONMENT OF THE ORGUEIL METEORITE PARENT BODY , 1963, Annals of the New York Academy of Sciences.

[9] E. Anders,et al. Chemical Evolution of the Carbonaceous Chondrites , 1962 .