Author/Authors :
Navrotsky، نويسنده , , Alexandra and Forray، نويسنده , , Ferenc Lلzلr and Drouet، نويسنده , , Christophe، نويسنده ,
Abstract :
Jarosite, a potassium (sodium) iron sulphate hydrated mineral, has recently been identified on the martian surface by the Opportunity rover. Using recent thermochemical data [Drouet and Navrotsky, 2003, Geochim. Cosmochim. Acta 67, 2063–2076; Forray et al., 2005, Geochim. Cosmochim. Acta, in press], we calculate the equilibrium decomposition curve of jarosite and show that it is thermodynamically stable under most present martian pressures and temperatures. Its stability makes jarosite potentially useful to retain textural, chemical, and isotopic evidence of past history, including possible biological activity, on Mars.
Keywords :
jarosite , mineral stability , Mars climate , Mineralogy