Js. Ray et R. Ramesh, A fluid-rock interaction model for carbon and oxygen isotopic variations in altered carbonatites, J GEOL S IN, 54(2), 1999, pp. 179-186
A fluid-rock interaction model for treating the stable carbon and oxygen is
otopic variations in altered carbonatites is presented and illustrated with
an example using data from the ferrocarbonatites of Amba Dongar, Gujarat.
The Amba Dongar ferrocarbonatites appear to have been altered by a fluid of
magmatic origin at 100 to 200 degrees C contrary to an earlier suggestion
of meteoric groundwater alteration at similar to 50 degrees C.