Stability and phase relations of nonstoichiometric clinopyroxenes in the join diopside-Ca-Eskola component at high pressures

Geochemistry International - Tập 45 - Trang 569-579 - 2007
N. V. Surkov1, Yu. G. Gartvich1, O. P. Izokh1
1Institute of Mineralogy and Petrography, Siberian Division, Russian Academy of Sciences, Novosibirsk, Russia

Tóm tắt

The stability of nonstoichiometric clinopyroxenes in the Di-CaEsk join was experimentally studied, and phase diagrams were constructed for this join at pressures of 2.0 and 3.0 GPa. It was found that melting in the diopside part of the join occurs at anomalously low temperatures, and nonstoichiometric clinopyroxene coexists with a phase approaching diopside in composition. Phase relations along the Di-CaEsk join can be described and consistently interpreted only assuming that the diopside phase (α-diopside) is thermodynamically stable. The following phase volumes were observed along the solidus of the join at a pressure of 3.0 GPa: Cpx, αDi+Cpx, αDi+Cpx+Qtz, αDi+Cpx+Grt+Qtz, Cpx+Grt+Qtz, Cpx+Grt+Ky+Qtz, Grt+Ky+Qtz. Melting occurs via the eutectic reaction αDi+Cpx+Grt+Qtz=L at a temperature of about 1200°C in the diopside part of the system and via the eutectic reaction Cpx+Grt+Ky+Qtz=L at a temperature of 1400°C in the calcium-rich part of the system. At a pressure of 2.0 GPa, melting occurs at temperatures of 1200–1300°C via the eutectic reaction αDi+Cpx+ An + Qtz=L. The invariant equilibrium (L, An, Cpx, Grt, αDi, Qtz) lies within the pressure range 2.0–3.0 GPa. Nonstoichiometric clinopyroxenes form complex solid solutions, the compositions of which are not strictly confined to the Di-CaEsk join and depend on temperature, pressure, and phase association. Grossular garnets coexist with nonstoichiometric clinopyroxenes and α-diopside.

Tài liệu tham khảo

N. V. Sobolev, Deep-Seated Inclusions in Kimberlites and the Problem of the Composition of the Upper Mantle, Ed. by V. S. Sobolev (Nauka, Novosibirsk, 1974; Am. Geophys. Union, Washington, DC, 1977). P. Eskola, “On the Eclogites of Norway,” Videnskaps Skr. J., Kristiania, i mat. Nat. kl. 8, 163–170 (1921). I. Kushiro, “Clinopyroxene Solid Solutions Formed by Reactions between Diopside and Plagioclase at High Pressures,” Mineral. Soc. Am. Spec. Pap. 2, 179–191 (1969). H. K. Mao, “The System Jadeite(NaAlSi2O6)-Anorthite at High Pressure,” Carnegie Inst. Wash. Yearbook 70, 163–170 (1971). V. A. Zharikov, I. P. Ivanov, Yu. A. Litvin, and R. A. Ishbulatov, “Experimental Study of the Melting of Calc-Alkaline Igneous Rocks at 35 Kbar,” Dokl. Akad. Nauk SSSR 219, 443–446 (1974). R. A. Ishbulatov, “Experimental Study of the Calc-Alkaline Series at 25–45 kbar,” in Contributions to Physicochemical Petrology (Nauka, Moscow, 1977), No. 6, pp. 97–167 [in Russian]. L. T. Khanukhova, V. A. Zharikov, R. A. Ishbulatov, and Yu. A. Litvin, “Excess Silica in High-Pressure Clinopyroxene Solid Solutions Based on Experimental Study of the System CaMgSi2O6-CaAl2SiO6-SiO2 at 35 kbar and 1200°C,” Dok. Akad. Nauk SSSR 229, 182–184 (1976). L. T. Khanukhova, V. A. Zharikov, R. A. Ishbulatov, and Yu. A. Litvin, “Pyroxene Solid Solutions in the System NaAlSi2O6-CaAl2SiO6-SiO2 at 35 kbar and 1200°C,” Dokl. Akad. Nauk SSSR 231, 185 (1976). L. T. Khanukhova, V. A. Zharikov, R. A. Ishbulatov, and Yu. A. Litvin, “The Silica Saturation Surface in the System CaMgSi2O6-NaAlSi2O6-CaAl2SiO6-SiO2 at 35 kbar and 1200°C,” Dokl. Akad. Nauk SSSR 234, 168–171 (1977). L. T. Khanukhova, “Experimental Study of the CaMgSi2O6-NaAlSi2O6-CaAl2SiO6-SiO2 System at 35 kbar and 1200C°,” in Contributions to Physicochemical Petrology (Nauka, Moscow, 1978), No. 8, pp. 155–178 [in Russian]. V. A. Zharikov, R. A. Ishbulatov, L. T. Chudinovskikh, and Yu. A. Litvin, “Solubility of Ca0.5AlSi2O6 End Member in Clinopyroxenes and the Problem of the Eclogitic barrier,” in Proceedings of All-Russia Symposium on Mantle Xenoliths and Problems of Ultramafic Magmas, Novosibirsk, Russia, 1980 (Novosibirsk, 1980), p. 88 [in Russian]. R. A. Ishbulatov, L. T. Chudinovskikh, and E. K. Malinovskaya, “Experimental Study of Solubility of the Ca0.5AlSi2O6 End Member in Clinopyroxenes at Pressure from 14 do 70 kbar,” in Proceedings of 13th Congress of International Mineralogical Association (IMA), Varna, Bulgaria, 1982 Ser. Bulg. Akad. Nauk. Crystallochem. Min., 351–357 (1986). E. K. Malinovskaya, A. M. Doroshev, V. K. Bulatov, and G. Brey, “Clinopyroxenes of the CaMgSi2O6-CaAl2SiO6-Ca0.5AlSi2O6 Series in Association with Anorthite, Quartz, Coesite, and Garnet,” Geokhimiya, No. 2, 216–226 (1991). B. J. Wood, “Mixing Properties of Tschermakitic Clinopyroxenes,” Am. Mineral. 61, 599–602 (1976). B. J. Wood and C. M. B. Henderson, “Compositions and Unit-Cell Parameters of Synthetic Non-Stoichiometric Tschermakitic Clinopyroxenes,” Am. Mineral. 63, 66–72 (1978). T. Gasparik and D. H. Lindsley, “Phase Equilibria at High Pressure of Pyroxenes Containing Monovalent and Trivalent Ions,” Mineral. Soc. Am. Rev. 7, 309–339 (1980). T. Gasparik, “Experimental Study of Subsolidus Phase Relations and Mixing Properties of Pyroxene in the System CaO-Al2O3-SiO2),” Geochim. Cosmochim. Acta 48, 2537–2545 (1984). T. Gasparik, “Experimental Study of Subsolidus Phase Relations and Mixing Properties of Clinopyroxene in the Silica-Saturated System CaO-MgO-Al2O3-SiO2,” Am. Mineral. 71, 686–693 (1986). N. V. Surkov, Yu. G. Gartvich, and Yu. V. Babich, “Experimental Study of the Phase Diagram of CaMgSi2O6-CaAl0.5Si2O6 System at 3.0 GPa,” Dokl. Akad. Nauk 398, 533–537 (2004) [Dokl. Earth Sci. 398, 1038–1042 (2004)]. F. R. Boyd and J. L. England, “Apparatus for Phase-Equilibrium Measurements at Pressures up to 50 Kilobars and Temperatures up to 1750°C,” J. Geophys. Res. 65, 741–748 (1960). A. A. Godovikov, S. A. Smirnov, I. Yu. Malinovskii, et al., “Apparatus for Measurements at Pressures up to 40 kbar and Temperatures up to 1700°C,” Prib. Tekhn. Eksp., No. 6, 159–160 (1971). P. W. Mirwald, I. C. Getting, and G. C. Kennedy, “Low-Friction Cell for Piston-Cylinder High-Pressure Apparatus,” J. Geophys. Res. 86, 1519–1525 (1975). N. V. Surkov, “A.s. SSSR. 1762458,” Byull. Izobret. 34, 213 (1992). N. V. Surkov and G. N. Kuznetsov, “Experimental Study of the Stability of Clinopyroxene Solid Solutions in the Assemblage Cpx+ Opx + Gr in the CaO-MgO-Al2O3-SiO2 System,” Geol. Geofiz. 37(12), 18–25 (1996). A. M. Doroshev, I. Yu. Malinovskii, N. V. Surkov, and A. A. Kalinin, “Attainment of Equilibrium between Clinopyroxene and Garnets in the System CaO-MgO-Al2O3-SiO2,” in Problems of Experiment in the High-Pressure Solid-Phase and Hydrothermal Apparatuses,” Ed. by I. I. Ivanov and Yu. A. Litvin (Nauka, Moscow, 1982) [in Russian]. A. M. Doroshev, N. V. Surkov, and I. Yu. Malinovskii, “Synthesis and Unit-Cell Parameters of Clinopyroxenes of the CaMgSi2O6-Mg2Si2O6 Series,” Zap. Vseross. Mineral. O-va, 110, 629–632 (1981). A. M. Doroshev, E. K. Malinovskaya, N. V. Surkov, and V. K. Bulatov, “Synthesis and Unit-Cell Parameters of Clinopyroxenes of the CaMgSi2O6-CaAl2SiO6 Series,” Geokhimiya, No. 12, 1755–1764 (1986). N. V. Surkov, “Stability of Aluminous Clinopyroxenes of the CaMgSi2O6-CaAl2SiO6 Series at High Pressures,” in Experimental Studies with Applications to the Problems of the Upper Mantle, Ed. by A. A. Godovikov, A. M. Doroshev, and I. Yu. Malinovskii (IGiG, Novosibirsk, 1982), pp. 51–62 [in Russian]. F. R. Boyd and J. K. England, “Effect of Pressure on the Melting of Diopside, CaMgSi2O6, and Albite, NaAlSi3O8, in the Range up to 50 Kilobars,” J. Geophys. Res. 68, 311–323 (1963). N. V. Surkov and A. M. Doroshev, “Phase Diagram of the CaO-Al2O3-SiO2 System at Pressures up to 40 kbar,” Geol. Geofiz. 39, 1254–1268 (1998).