Cubic FeS, a Metastable Iron Sulfide
- 11 December 1970
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 170 (3963) , 1191-1192
- https://doi.org/10.1126/science.170.3963.1191
Abstract
Studies of the corrosion products of metallic iron formed in the absence of air oxidation in solutions of hydrogen sulfide have revealed the existence of a new phase, cubic FeS, associated with tetragonal iron sulfide, Fe1 + xS. This new phase is metastable and has a sphalerite-like structure.Keywords
This publication has 5 references indexed in Scilit:
- thermodynamic stability of sedimentary iron sulfidesAmerican Journal of Science, 1967
- Phase relations involving sphalerite in the Fe-Zn-S systemEconomic Geology, 1966
- Crystallographic Study of Chromium SpinelsJournal of Applied Physics, 1966
- Iron Sulfides Formed from Aqueous Solution at Low Temperatures and Atmospheric PressureThe Journal of Geology, 1964
- Tetragonal Iron SulfideScience, 1962