Delgado, J.Soler Gil, AlbertArcos, D.2017-01-252017-01-251996http://hdl.handle.net/10272/13159The isotopic composition of carbonates related to the skarn and contact metamorphic aureole of La Maladeta batholith show a broad range of variation. The whole set of obtained data can be modeled by means of an isotopic exchange between a fluid equilibrated with a magma, with an isotopic composition of ô '“O smow =8-5% o and unknow S IJCmB at Xco, < 0 . 0 2 and a Devonian limestone of 8 laO Mnw= 2 8 -29%o 8 I3Cpdi=4-5%o Volatilization processes have been observed previosly to isotopic exchangespaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/CO. stable isotopesGeochemistry,SkarnHercynianPyreneesjournal articleopen access