Compositions of clinopyroxene solid solutions in Di-CaEs section of CMAS system at pressure up to 3.0 GPa
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Abstract
The possibility of ‘excess’ silica dissolution in clinopyroxene as calcium molecule of Eskola (CaEs) end member has been known for a long time. At present time attempts to determine the dependence of such non-stoichiometric clinopyroxene compositions on (P, T)-parameters are continued. In this article Di-CaEs section of ‘dry’ CMAS system was investigated in P-T range of up to 3.0 GPa and up to 1550 o C. Experiments with synthetic clinopyroxene compositions were carried out on a vertical shaft electric resistance furnace with silicon carbide heaters (at atmospheric pressure) and were run by quenching method on the piston-cylinder apparatus (at high pressure). It was found that two independent stable pyroxene phases are formed: aluminous clinopyroxene and a high-magnesian alumina-free diopside. It was clarified that clinopyroxene solid solution is represented by a quad series of Di-En-CaTs-CaEs end members. It was shown that diopside phase belongs to Di-En solid solution. A tetrahedron of clinopyroxene compositions was constructed, occupying a central position in CMAS system. Experimental data obtained can serve as a necessary model for subsequent studying influence of alkalis, ferruginous component, etc. on stability of quartz-normative mineral associations and identical ‘real’ parageneses.
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