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Correction to “Thermal decomposition of carbonates in fault zones: Slip‐weakening and temperature‐limiting effects”
Author(s) -
Sulem J.,
Famin V.,
Noda H.
Publication year - 2009
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2009jb006576
Subject(s) - cabin pressurization , pore water pressure , slip (aerodynamics) , limiting , materials science , thermal , microscale chemistry , endothermic process , thermodynamics , mechanics , geology , geotechnical engineering , composite material , chemistry , mechanical engineering , physics , mathematics education , mathematics , engineering , organic chemistry , adsorption
International audienceIn the paper ‘‘Thermal decomposition of carbonates in fault zones: Slip-weakening and temperature-limiting effects’’ by Sulem and Famin (Journal of Geophysical Research, 114, B03309, doi:10.1029/2008JB006004, 2009), the mass of CaO produced in the chemical reaction of calcite decomposition (decarbonation) CaCO3 → CaO+CO2 was neglected. Following a remark of H. Noda (private communication, 2009), this term can be taken intoaccount in themass balance of the solid phas

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