Carbonation of peridotites and decarbonation of siliceous dolomites represented in the system CaO-MgO-SiO2-CO2 to 30 kbar
- 1 December 1983
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 100 (1-3), 359-388
- https://doi.org/10.1016/0040-1951(83)90194-4
Abstract
No abstract availableKeywords
This publication has 33 references indexed in Scilit:
- Pyroxene-carbonate reactions in the upper mantleEarth and Planetary Science Letters, 1983
- The effect of CO<2) upon partial melting of peridotite in the system Na<2) O-CaO-Al<2) O<3) -MgO-SiO<2) -CO<2) to 35 kb, with an analysis of melting in a peridotite-H<2) O-CO<2) systemAmerican Journal of Science, 1978
- Does CO2 cause partial melting in the low-velocity layer of the mantle?: Comment and replyGeology, 1976
- Carbonate-silicate reactions at high presures and possible presence of dolomite and magnesite in the upper mantleEarth and Planetary Science Letters, 1975
- Melting Reactions in the System NaAlSi3O8-KAlSi3O8-SiO2 to 35 Kilobars, Dry and with Excess WaterThe Journal of Geology, 1975
- Stability of forsterite + CO2 and its bearing on the role of CO2 in the mantleEarth and Planetary Science Letters, 1975
- Experimental Data for Reactions in Siliceous MarblesThe Journal of Geology, 1971
- An experimental investigation of the system MgO-SiO 2 -H 2 O-CO 2American Journal of Science, 1969
- Subsolidus Phase Relations in the System CaCO3-MgCO3The Journal of Geology, 1961
- A Thermochemical Study of Equilibrium Relations during Metamorphism of Siliceous Carbonate RocksThe Journal of Geology, 1956