Shock-induced CO2 loss from CaCO3; implications for early planetary atmospheres

Earth and Planetary Science Letters

Volumn 77, Issue 3-4, 1986, Pages 409-418

  Lange, Manfred A ^a   Ahrens, Thomas J ^a  

^a Seismological Laboratory 252 21 California Institute of Technology Pasadena CA 91125 USA ^*

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0022463141     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/0012-821X(86)90150-0     Document Type: Article

References (27)

1. Chemical structure of the Earth's crust
2. The role of volatiles and lithology in the impact cratering process
3. Carbonate formation in mars-like environment
4. Oxidation state of the atmosphere and crust of Venus from Pioneer-Venus results
5. The evolution of an impact-generated atmosphere
6. Impact-induced dehydration of serpentine and the evolution of planetary atmospheres
7. 2O and the homogeneous accretion of the earth
8. Origin of the ocean
9. The mineralogy of meteorites
10. Carbon, hydrogen, and nitrogen isotopes in solvent-extractable organic matter from carbonaceous chondrites
11. Carbon chemistry of separated phases of Murchison and Allende meteorites (abstract)
12. The evolution of the atmosphere of the earth
13. Some standard thermal dehydration curves of minerals
14. Micas in experimentally shocked gneiss
15. The evolution of an impact-generated atmosphere (abstract)
16. Heterogeneous shock-induced thermal radiation in minerals
17. Processes occurring in shock compression of rocks and minerals
18. A study of the volumetric compressibility of marble at high pressures
19. Dynamic compression and volatile release of carbonates
20. The equation of state of solids from shock wave studies
21. 2 to 33 kilobars