Cubanite: A New Sulfide Phase in CI Meteorites
- 5 August 1977
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 197 (4303) , 561-562
- https://doi.org/10.1126/science.197.4303.561
Abstract
Cubanite (CuFe 2 S 3 ), 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.Keywords
This publication has 12 references indexed in Scilit:
- Mafic silicates in the Orgueil carbonaceous meteoriteEarth and Planetary Science Letters, 1976
- Major element composition of phyllosilicates in the Orgueil carbonaceous meteoriteEarth and Planetary Science Letters, 1976
- Low temperature condensation from the solar nebulaIcarus, 1972
- METEORITIC PYRRHOTITEMeteoritics, 1970
- Chemical fractionations in meteorites—II. Abundance patterns and their interpretationGeochimica et Cosmochimica Acta, 1967
- A chemical-petrologic classification for the chondritic meteoritesGeochimica et Cosmochimica Acta, 1967
- Thermal Stability of Assemblages in the Cu--Fe--S SystemJournal of Petrology, 1966
- LOW‐TEMPERATURE MINERALS FROM THE FINE‐GRAINED MATRIX OF SOME CARBONACEOUS METEORITESAnnals of the New York Academy of Sciences, 1964
- AQUEOUS, LOW TEMPERATURE ENVIRONMENT OF THE ORGUEIL METEORITE PARENT BODYAnnals of the New York Academy of Sciences, 1963
- On the chemical evolution of the carbonaceous chondritesGeochimica et Cosmochimica Acta, 1962