Pyrite: Shock compression, isentropic release, and composition of the Earth's core
Open Access
- 10 September 1987
- journal article
- regular section
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 92 (B10) , 10363-10375
- https://doi.org/10.1029/jb092ib10p10363
Abstract
No abstract availableKeywords
This publication has 46 references indexed in Scilit:
- Shock-induced CO2 loss from CaCO3; implications for early planetary atmospheresEarth and Planetary Science Letters, 1986
- FeO and H2O and the homogeneous accretion of the earthEarth and Planetary Science Letters, 1984
- Composition of the core, II. Effect of high pressure on solubility of FeO in molten ironEarth and Planetary Science Letters, 1984
- Hydrogen in the earth's core. Experimental approach.Proceedings of the Japan Academy, Series B, 1983
- Limited aperture light source streak photographyReview of Scientific Instruments, 1982
- Models of the Earth's CoreScience, 1981
- Preliminary reference Earth modelPhysics of the Earth and Planetary Interiors, 1981
- Shock compression of aluminum, copper, and tantalumJournal of Applied Physics, 1981
- High-pressure polymorphism of the iron oxidesGeophysical Journal of the Royal Astronomical Society, 1981
- The Deep-Earth-Gas HypothesisScientific American, 1980