Experimental study of the system diopside–nepheline–sanidine at 0.1, 1 and 2 GPa [P(H2O) = P(Total)]: Its significance in the genesis of alkali-rich basic and ultrabasic rocks

Bulk compositions of nephelinite, melanephelinite, trachyte and phonolite can be represented in the join diopside–nepheline–sanidine, which is a part of the quinary system, nepheline–kalsilite–CaO–MgO–SiO2. Thirty-two starting compositions were made in this join. Experiments were conducted on these compositions at 0.1, 1 and 2 GPa [P(H2O) = P(Total)] and variable temperatures to investigate phase equilibria relations. In the present study, we determined the compositions and temperatures of equilibrium of the four-phase points in the diopside–nepheline–sanidine join at [0.1, 1 and 2 GPa P(H2O) = P(Total)]. All phases are found to be solid solutions. At 0.1 GPa, the join intersects the primary phase volume of forsterite solid solution. Two four-phase points were established, one at Diopside26Nepheline66Sanidine8 and 990 °C where liquid co-exists with forsterite solid solution + diopside solid solution + nepheline solid solution and the other point at Diopside11Nepheline31Sanidine58 and 865 °C at which diopside solid solution + nepheline solid solution + leucite solid solution is a stable suprasolidus phase assemblage. At 1 GPa liquid co-exists with diopside solid solution + nepheline solid solution + sanidine solid solution at Diopside4Sanidine65Nepheline31 and 670 °C. The four-phase point (diopside solid solution + nepheline solid solution + sanidine solid solution + liquid) at 2 GPa was located at Diopside3Sanidine73Nepheline24.The results at 0.1 GPa show that a nepheline-bearing leucitite can be derived from a leucitite, a nepheline-bearing italite or an olivine-bearing nephelinite by crustal differentiation processes. After reaction with liquid, leucite disappears at 815 °C near the solidus, and the final assemblage corresponds to a pyroxene-bearing phonolite.The present experimental results at 1 and 2 GPa suggest that a pyroxene-bearing phonolite can be generated either from a pyroxene trachyte or a nephelinite or a pyroxene-poor phonolite magma, and a phonolite melt itself can be derived at depths 30–35 (1 GPa) or 60–65 km (∼ 2 GPa).