Petrology of Venus: Further Deductions
- 13 March 1964
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 143 (3611), 1161
- https://doi.org/10.1126/science.143.3611.1161.a
Abstract
The carbon dioxide pressure of the atmosphere of Venus may be controlled by one or more of several decarbonation reactions. One of these is the formation of carbonate-rich liquids. The pressure-temperature equilibrium conditions of these reactions are in the range of those proposed for the surface of Venus.Keywords
This publication has 6 references indexed in Scilit:
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- The System CaO-CO2-H2O and the Origin of CarbonatitesJournal of Petrology, 1960
- A Thermochemical Study of Equilibrium Relations during Metamorphism of Siliceous Carbonate RocksThe Journal of Geology, 1956
- Progressive Metamorphism of Siliceous Limestone and DolomiteThe Journal of Geology, 1940