Skip to main content

2014 | OriginalPaper | Buchkapitel

4. System CaO–MgO–SiO2

verfasst von : Professor Tibor Gasparik

Erschienen in: Phase Diagrams for Geoscientists

Verlag: Springer New York

Aktivieren Sie unsere intelligente Suche um passende Fachinhalte oder Patente zu finden.

search-config
loading …

Abstract

The main focus in this chapter is on the enstatite-diopside join, which includes petrologically most important compositions in the CMS system, and is, undoubtedly, the most thoroughly investigated binary join in the experimental petrology. The earlier investigations concentrated mainly on the subsolidus phase relations since the data of Davis and Boyd [155] suggested that the compositions of the coexisting orthopyroxene and clinopyroxene are primarily temperature dependent and thus suitable as a geothermometer. The first experimental data at 1 atm were reported by Atlas [91], Boyd and Shairer [118], Kushiro [287], Yang and Foster [469], and Yang [468]. Later studies at 1 atm were conducted to elucidate the stability of the second field of orthopyroxene found at high temperatures [99, 172, 253, 305]. First subsolidus data at high pressures were reported by Warner and Luth [439], Mori and Green [329], and Lindsley and Dixon [296]. A good summary of these studies was given by Carlson [132] and Carlson and Lindsley [134].

Sie haben noch keine Lizenz? Dann Informieren Sie sich jetzt über unsere Produkte:

Springer Professional "Wirtschaft+Technik"

Online-Abonnement

Mit Springer Professional "Wirtschaft+Technik" erhalten Sie Zugriff auf:

  • über 102.000 Bücher
  • über 537 Zeitschriften

aus folgenden Fachgebieten:

  • Automobil + Motoren
  • Bauwesen + Immobilien
  • Business IT + Informatik
  • Elektrotechnik + Elektronik
  • Energie + Nachhaltigkeit
  • Finance + Banking
  • Management + Führung
  • Marketing + Vertrieb
  • Maschinenbau + Werkstoffe
  • Versicherung + Risiko

Jetzt Wissensvorsprung sichern!

Springer Professional "Technik"

Online-Abonnement

Mit Springer Professional "Technik" erhalten Sie Zugriff auf:

  • über 67.000 Bücher
  • über 390 Zeitschriften

aus folgenden Fachgebieten:

  • Automobil + Motoren
  • Bauwesen + Immobilien
  • Business IT + Informatik
  • Elektrotechnik + Elektronik
  • Energie + Nachhaltigkeit
  • Maschinenbau + Werkstoffe




 

Jetzt Wissensvorsprung sichern!

Literatur
15.
Zurück zum Zitat Gasparik, T.: Transformation of enstatite-diopside-jadeite pyroxenes to garnet. Contrib. Miner. Petrol. 102, 389–405 (1989)CrossRef Gasparik, T.: Transformation of enstatite-diopside-jadeite pyroxenes to garnet. Contrib. Miner. Petrol. 102, 389–405 (1989)CrossRef
19.
Zurück zum Zitat Gasparik, T.: A thermodynamic model for the enstatite-diopside join. Am. Mineral. 75, 1080–1091 (1990) Gasparik, T.: A thermodynamic model for the enstatite-diopside join. Am. Mineral. 75, 1080–1091 (1990)
21.
Zurück zum Zitat Gasparik, T.: Phase relations in the transition zone. J. Geophys. Res. 95, 15751–15769 (1990)CrossRef Gasparik, T.: Phase relations in the transition zone. J. Geophys. Res. 95, 15751–15769 (1990)CrossRef
24.
Zurück zum Zitat Presnall, D.C., Gasparik, T.: Melting of enstatite (MgSiO3) from 10 to 16.5 GPa and the forsterite (Mg2SiO4) – majorite (MgSiO3) eutectic at 16.5 GPa: implications for the origin of the mantle. J. Geophys. Res. 95, 15771–15777 (1990)CrossRef Presnall, D.C., Gasparik, T.: Melting of enstatite (MgSiO3) from 10 to 16.5 GPa and the forsterite (Mg2SiO4) – majorite (MgSiO3) eutectic at 16.5 GPa: implications for the origin of the mantle. J. Geophys. Res. 95, 15771–15777 (1990)CrossRef
26.
Zurück zum Zitat Herzberg, C., Gasparik, T.: Garnet and pyroxenes in the mantle: a test of the majorite fractionation hypothesis. J. Geophys. Res. 96, 16263–16274 (1991)CrossRef Herzberg, C., Gasparik, T.: Garnet and pyroxenes in the mantle: a test of the majorite fractionation hypothesis. J. Geophys. Res. 96, 16263–16274 (1991)CrossRef
38.
Zurück zum Zitat Gasparik, T., Wolf, K., Smith, C.M.: Experimental determination of phase relations in the CaSiO3 system from 8 to 15 GPa. Am. Mineral. 79, 1219–1222 (1994) Gasparik, T., Wolf, K., Smith, C.M.: Experimental determination of phase relations in the CaSiO3 system from 8 to 15 GPa. Am. Mineral. 79, 1219–1222 (1994)
40.
Zurück zum Zitat Hazen, R.M., Downs, R.T., Finger, L.W., Conrad, P.G., Gasparik, T.: Crystal chemistry of cabearing majorite. Am. Mineral. 79, 581–584 (1994) Hazen, R.M., Downs, R.T., Finger, L.W., Conrad, P.G., Gasparik, T.: Crystal chemistry of cabearing majorite. Am. Mineral. 79, 581–584 (1994)
44.
Zurück zum Zitat Gasparik, T.: Melting experiments on the enstatite-diopside join at 70–224 kbar, including the melting of diopside. Contrib. Miner. Petrol. 124, 139–153 (1996)CrossRef Gasparik, T.: Melting experiments on the enstatite-diopside join at 70–224 kbar, including the melting of diopside. Contrib. Miner. Petrol. 124, 139–153 (1996)CrossRef
82.
Zurück zum Zitat Anastasiou, P., Seifert, F.: Solid solubility of Al2O3 in enstatite at high temperatures and 1–5 kb water pressure. Contrib. Miner. Petrol. 34, 272–287 (1972)CrossRef Anastasiou, P., Seifert, F.: Solid solubility of Al2O3 in enstatite at high temperatures and 1–5 kb water pressure. Contrib. Miner. Petrol. 34, 272–287 (1972)CrossRef
90.
Zurück zum Zitat Atlas, L.: The polymorphism of MgSiO3 and solid-state equilibria in the system MgSiO3–CaMgSi2O6. J. Geol. 60, 125–147 (1952)CrossRef Atlas, L.: The polymorphism of MgSiO3 and solid-state equilibria in the system MgSiO3–CaMgSi2O6. J. Geol. 60, 125–147 (1952)CrossRef
98.
Zurück zum Zitat Biggar, G.M.: Calcium-poor pyroxenes: phase relations in the system CaO–MgO–Al2O3–SiO2. Miner. Mag. 49, 49–58 (1985)CrossRef Biggar, G.M.: Calcium-poor pyroxenes: phase relations in the system CaO–MgO–Al2O3–SiO2. Miner. Mag. 49, 49–58 (1985)CrossRef
99.
Zurück zum Zitat Biggar, G.M.: Protoenstatite compositions from 1 bar to 5 kb (abs). Chem. Geol. 70, 3 (1988)CrossRef Biggar, G.M.: Protoenstatite compositions from 1 bar to 5 kb (abs). Chem. Geol. 70, 3 (1988)CrossRef
110.
Zurück zum Zitat Bowen, N.L.: The ternary system diopside-forsterite-silica. Am. J. Sci. 38, 207–264 (1914)CrossRef Bowen, N.L.: The ternary system diopside-forsterite-silica. Am. J. Sci. 38, 207–264 (1914)CrossRef
114.
Zurück zum Zitat Boyd, F.R., England, J.L.: 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)CrossRef Boyd, F.R., England, J.L.: 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)CrossRef
117.
Zurück zum Zitat Boyd, F.R., Shairer, J.F.: The system MgSiO3–CaMgSi2O6. J. Petrol. 5, 275–309 (1964)CrossRef Boyd, F.R., Shairer, J.F.: The system MgSiO3–CaMgSi2O6. J. Petrol. 5, 275–309 (1964)CrossRef
118.
Zurück zum Zitat Boyd, F.R., England, J.L., Davis, B.T.C.: Effects of pressure on the melting and polymorphism of enstatite, MgSiO3. J. Geophys. Res. 69, 2101–2109 (1964)CrossRef Boyd, F.R., England, J.L., Davis, B.T.C.: Effects of pressure on the melting and polymorphism of enstatite, MgSiO3. J. Geophys. Res. 69, 2101–2109 (1964)CrossRef
120.
Zurück zum Zitat Brey, G., Huth, J.: The enstatite-diopside solvus to 60 kbar. Proceed Third Inter Kimberlite Conf. 2, 257–264 (1984) Brey, G., Huth, J.: The enstatite-diopside solvus to 60 kbar. Proceed Third Inter Kimberlite Conf. 2, 257–264 (1984)
127.
Zurück zum Zitat Canil, D.: Stability of clinopyroxene at pressure-temperature conditions of the transition zone. Phys. Earth. Planet. Inter. 86, 25–34 (1994)CrossRef Canil, D.: Stability of clinopyroxene at pressure-temperature conditions of the transition zone. Phys. Earth. Planet. Inter. 86, 25–34 (1994)CrossRef
129.
Zurück zum Zitat Carlson, W.D.: Evidence against the stability of orthoenstatite above 1005°C at atmospheric pressure in CaO–MgO–SiO2. Geophys. Res. Lett. 12, 409–411 (1985)CrossRef Carlson, W.D.: Evidence against the stability of orthoenstatite above 1005°C at atmospheric pressure in CaO–MgO–SiO2. Geophys. Res. Lett. 12, 409–411 (1985)CrossRef
130.
Zurück zum Zitat Carlson, W.D.: Reversed pyroxene phase equilibria in CaO–MgO–SiO2 at one atmosphere pressure. Contrib. Miner. Petrol. 92, 218–224 (1986)CrossRef Carlson, W.D.: Reversed pyroxene phase equilibria in CaO–MgO–SiO2 at one atmosphere pressure. Contrib. Miner. Petrol. 92, 218–224 (1986)CrossRef
131.
Zurück zum Zitat Carlson, W.D.: Subsolidus phase equilibria on the forsterite-saturated join Mg2Si2O6–CaMgSi2O6 at atmospheric pressure. Am. Mineral. 73, 232–241 (1988) Carlson, W.D.: Subsolidus phase equilibria on the forsterite-saturated join Mg2Si2O6–CaMgSi2O6 at atmospheric pressure. Am. Mineral. 73, 232–241 (1988)
133.
Zurück zum Zitat Carlson, W.D., Lindsley, D.H.: Thermochemistry of pyroxenes on the join Mg2Si2O6–CaMgSi2O6. Am. Mineral. 73, 242–252 (1988) Carlson, W.D., Lindsley, D.H.: Thermochemistry of pyroxenes on the join Mg2Si2O6–CaMgSi2O6. Am. Mineral. 73, 242–252 (1988)
134.
Zurück zum Zitat Carlson, W.D., Swinnea, J.S., Miser, D.E.: Stability of orthoenstatite at high temperature and low pressure. Am. Mineral. 73, 1255–1263 (1988) Carlson, W.D., Swinnea, J.S., Miser, D.E.: Stability of orthoenstatite at high temperature and low pressure. Am. Mineral. 73, 1255–1263 (1988)
145.
Zurück zum Zitat Chen, C.-H., Presnall, D.C.: The system Mg2SiO4-SiO2 at pressures up to 25 kilobars. Am. Mineral. 60, 398–406 (1975) Chen, C.-H., Presnall, D.C.: The system Mg2SiO4-SiO2 at pressures up to 25 kilobars. Am. Mineral. 60, 398–406 (1975)
153.
Zurück zum Zitat Davidson, P.M., Lindsley, D.H., Carlson, W.D.: Thermochemistry of pyroxenes on the join Mg2Si2O6–CaMgSi2O6: a revision of the model for pressures up to 30 kbar. Am. Mineral. 73, 1264–1266 (1988) Davidson, P.M., Lindsley, D.H., Carlson, W.D.: Thermochemistry of pyroxenes on the join Mg2Si2O6–CaMgSi2O6: a revision of the model for pressures up to 30 kbar. Am. Mineral. 73, 1264–1266 (1988)
154.
Zurück zum Zitat Davis, B.T.C., Boyd, F.R.: The join Mg2Si2O6–CaMgSi2O6 at 30 kilobars pressure and its application to pyroxenes from kimberlites. J. Geophys. Res. 71, 3567–3576 (1966)CrossRef Davis, B.T.C., Boyd, F.R.: The join Mg2Si2O6–CaMgSi2O6 at 30 kilobars pressure and its application to pyroxenes from kimberlites. J. Geophys. Res. 71, 3567–3576 (1966)CrossRef
165.
Zurück zum Zitat Essene, E.: High-pressure transformations in CaSiO3. Contrib. Miner. Pet 45, 247–250 (1974)CrossRef Essene, E.: High-pressure transformations in CaSiO3. Contrib. Miner. Pet 45, 247–250 (1974)CrossRef
171.
Zurück zum Zitat Foster, W.R., Lin, H.C.: New data on the forsterite-diopside-silica system. Eos. Trans. AGU. 56, 470 (1975) Foster, W.R., Lin, H.C.: New data on the forsterite-diopside-silica system. Eos. Trans. AGU. 56, 470 (1975)
226.
Zurück zum Zitat Howells, S., O’Hara, M.J.: Palaeogeotherms and the diopside-enstatite solvus. Nature 254, 406–408 (1975)CrossRef Howells, S., O’Hara, M.J.: Palaeogeotherms and the diopside-enstatite solvus. Nature 254, 406–408 (1975)CrossRef
239.
Zurück zum Zitat Irifune, T., Ohtani, E.: Melting of pyrope Mg3Al2Si3O12 up to 10 GPa: possibility of a pressureinduced structural change in pyrope melt. J. Geophys. Res. 91, 9357–9366 (1986)CrossRef Irifune, T., Ohtani, E.: Melting of pyrope Mg3Al2Si3O12 up to 10 GPa: possibility of a pressureinduced structural change in pyrope melt. J. Geophys. Res. 91, 9357–9366 (1986)CrossRef
242.
Zurück zum Zitat Irifune, T., Susaki, J., Yagi, T., Sawamoto, H.: Phase transformations in diopside CaMgSi2O6 at pressures up to 25 GPa. Geophys. Res. Lett. 16, 187–190 (1989)CrossRef Irifune, T., Susaki, J., Yagi, T., Sawamoto, H.: Phase transformations in diopside CaMgSi2O6 at pressures up to 25 GPa. Geophys. Res. Lett. 16, 187–190 (1989)CrossRef
252.
Zurück zum Zitat Jenner, G.A., Green, D.H.: Equilibria in the Mg-rich part of the pyroxene quadrilateral. Miner. Mag. 47, 153–160 (1983)CrossRef Jenner, G.A., Green, D.H.: Equilibria in the Mg-rich part of the pyroxene quadrilateral. Miner. Mag. 47, 153–160 (1983)CrossRef
260.
Zurück zum Zitat Kanzaki, M., Stebbins, J.F., Xue, X.: Characterization of quenched high pressure phases in Ca- SiO3 system by XRD and 29Si NMR. Geophys. Res. Lett. 18, 463–466 (1991)CrossRef Kanzaki, M., Stebbins, J.F., Xue, X.: Characterization of quenched high pressure phases in Ca- SiO3 system by XRD and 29Si NMR. Geophys. Res. Lett. 18, 463–466 (1991)CrossRef
281.
Zurück zum Zitat Kushiro, I.: Wollastonite-pseudowollastonite inversion. Carnegie. Inst. Wash. Yearb. 63, 83–84 (1964) Kushiro, I.: Wollastonite-pseudowollastonite inversion. Carnegie. Inst. Wash. Yearb. 63, 83–84 (1964)
284.
Zurück zum Zitat Kushiro, I.: The system forsterite-diopside-silica with and without water at high pressures. Am. J. Sci. 267-A, 269–294 (1969) Kushiro, I.: The system forsterite-diopside-silica with and without water at high pressures. Am. J. Sci. 267-A, 269–294 (1969)
286.
Zurück zum Zitat Kushiro, I.: Determination of liquidus relations in synthetic silicate systems with electron probe analysis: the system forsterite-diopside-silica at 1 atmosphere. Am. Mineral. 57, 1260–1271 (1972) Kushiro, I.: Determination of liquidus relations in synthetic silicate systems with electron probe analysis: the system forsterite-diopside-silica at 1 atmosphere. Am. Mineral. 57, 1260–1271 (1972)
294.
Zurück zum Zitat Lindsley, D.H.: Phase equilibria of pyroxenes at pressures > 1 atmosphere. In: Prewitt, C.T. (ed.) Reviews in Mineralogy. Pyroxenes, vol. 7, pp. 289–307. Mineralogical Society of America, Washington DC (1980) Lindsley, D.H.: Phase equilibria of pyroxenes at pressures > 1 atmosphere. In: Prewitt, C.T. (ed.) Reviews in Mineralogy. Pyroxenes, vol. 7, pp. 289–307. Mineralogical Society of America, Washington DC (1980)
295.
Zurück zum Zitat Lindsley, D.H., Dixon, S.A.: Diopside-enstatite equilibria at 850 to 1400°C, 5–35 kbars. Am. J. Sci. 276, 1285–1301 (1976)CrossRef Lindsley, D.H., Dixon, S.A.: Diopside-enstatite equilibria at 850 to 1400°C, 5–35 kbars. Am. J. Sci. 276, 1285–1301 (1976)CrossRef
297.
Zurück zum Zitat Lindsley, D.H., Grover, J.E., Davidson, P.M.: The thermodynamics of the Mg2Si2O6–CaMgSi2O6 join: a review and an improved model. In: Newton, R.C., Navrotsky, A., Wood, B.J. (eds.) Thermodynamics of Minerals and Melts, pp. 149–175. Springer-Verlag, New York (1981)CrossRef Lindsley, D.H., Grover, J.E., Davidson, P.M.: The thermodynamics of the Mg2Si2O6–CaMgSi2O6 join: a review and an improved model. In: Newton, R.C., Navrotsky, A., Wood, B.J. (eds.) Thermodynamics of Minerals and Melts, pp. 149–175. Springer-Verlag, New York (1981)CrossRef
304.
Zurück zum Zitat Longhi, J., Boudreau, A.E.: The orthoenstatite liquidus field in the system forsterite-diopside-silica at one atmosphere. Am. Mineral. 65, 563–573 (1980) Longhi, J., Boudreau, A.E.: The orthoenstatite liquidus field in the system forsterite-diopside-silica at one atmosphere. Am. Mineral. 65, 563–573 (1980)
308.
Zurück zum Zitat Malavergne, V., Guyot, F., Benzerara, K., Martinez, I.: Description of new shock-induced phases in the Shergotty, Zagami, Nakhla and Chassigny meteorites. Meteorit. Planet. Sci. 36, 1297–1305 (2001)CrossRef Malavergne, V., Guyot, F., Benzerara, K., Martinez, I.: Description of new shock-induced phases in the Shergotty, Zagami, Nakhla and Chassigny meteorites. Meteorit. Planet. Sci. 36, 1297–1305 (2001)CrossRef
313.
Zurück zum Zitat Mao, H.K., Yagi, T., Bell, P.M.: Mineralogy of the earth’s deep mantle: quenching experiments on mineral compositions at high pressure and temperature. Carnegie. Inst. Wash. Yearb. 76, 502–504 (1977) Mao, H.K., Yagi, T., Bell, P.M.: Mineralogy of the earth’s deep mantle: quenching experiments on mineral compositions at high pressure and temperature. Carnegie. Inst. Wash. Yearb. 76, 502–504 (1977)
328.
Zurück zum Zitat Mori, T., Green, D.H.: Pyroxenes in the system Mg2Si2O6–CaMgSi2O6 at high pressure. Earth. Planet. Sci. Lett. 26, 277–286 (1975)CrossRef Mori, T., Green, D.H.: Pyroxenes in the system Mg2Si2O6–CaMgSi2O6 at high pressure. Earth. Planet. Sci. Lett. 26, 277–286 (1975)CrossRef
329.
Zurück zum Zitat Mori, T., Green, D.H.: Subsolidus equilibria between pyroxenes in the CaO–MgO–SiO2 system at high pressures and temperatures. Am. Mineral. 61, 616–625 (1976) Mori, T., Green, D.H.: Subsolidus equilibria between pyroxenes in the CaO–MgO–SiO2 system at high pressures and temperatures. Am. Mineral. 61, 616–625 (1976)
338.
Zurück zum Zitat Nickel, K.G., Brey, G.: Subsolidus orthopyroxene-clinopyroxene systematics in the system CaO–MgO–SiO2 to 60 kbar: a re-evaluation of the regular solution model. Contrib. Miner. Pet. 87, 35–42 (1984)CrossRef Nickel, K.G., Brey, G.: Subsolidus orthopyroxene-clinopyroxene systematics in the system CaO–MgO–SiO2 to 60 kbar: a re-evaluation of the regular solution model. Contrib. Miner. Pet. 87, 35–42 (1984)CrossRef
348.
Zurück zum Zitat Osborn, E.F., Shairer, J.F.: The ternary system pseudowollastonite-åkermanite-gehlenite. Am. J. Sci. 239, 715–763 (1941)CrossRef Osborn, E.F., Shairer, J.F.: The ternary system pseudowollastonite-åkermanite-gehlenite. Am. J. Sci. 239, 715–763 (1941)CrossRef
394.
Zurück zum Zitat Scarfe, C.M., Takahashi, E.: Melting of garnet peridotite to 13 GPa and the early history of the upper mantle. Nature 322, 354–356 (1986)CrossRef Scarfe, C.M., Takahashi, E.: Melting of garnet peridotite to 13 GPa and the early history of the upper mantle. Nature 322, 354–356 (1986)CrossRef
400.
Zurück zum Zitat Schweitzer, E.: The reaction pigeonite = diopsidess + enstatitess at 15 kbars. Am. Mineral. 67, 54–58 (1982) Schweitzer, E.: The reaction pigeonite = diopsidess + enstatitess at 15 kbars. Am. Mineral. 67, 54–58 (1982)
408.
Zurück zum Zitat Shen, G., Lazor, P.: Measurement of melting temperatures of some minerals under lower mantle pressures. J. Geophys. Res. 100, 17699–17713 (1995)CrossRef Shen, G., Lazor, P.: Measurement of melting temperatures of some minerals under lower mantle pressures. J. Geophys. Res. 100, 17699–17713 (1995)CrossRef
410.
Zurück zum Zitat Simon, F.E., Glatzel, G.: Remarks on the fusion-pressure curve. Z. Anorg. Allg. Chemie. 178, 309–316 (1929)CrossRef Simon, F.E., Glatzel, G.: Remarks on the fusion-pressure curve. Z. Anorg. Allg. Chemie. 178, 309–316 (1929)CrossRef
428.
Zurück zum Zitat Tamai, H., Yagi, T.: High-pressure and high-temperature phase relations in CaSiO3 and CaMgSi2O6, and elasticity of perovskite-type CaSiO3. Phys. Earth. Planet. Inter. 54, 370–377 (1989)CrossRef Tamai, H., Yagi, T.: High-pressure and high-temperature phase relations in CaSiO3 and CaMgSi2O6, and elasticity of perovskite-type CaSiO3. Phys. Earth. Planet. Inter. 54, 370–377 (1989)CrossRef
438.
Zurück zum Zitat Warner, R.D., Luth, W.L.: The diopside-orthoenstatite two-phase region in the system CaMgSi2O6–Mg2Si2O6. Am. Mineral. 59, 98–109 (1974) Warner, R.D., Luth, W.L.: The diopside-orthoenstatite two-phase region in the system CaMgSi2O6–Mg2Si2O6. Am. Mineral. 59, 98–109 (1974)
443.
Zurück zum Zitat Wang, Y., Weidner, D.J.: Thermoelasticity of CaSiO3 perovskite and implications for the lower mantle. Geophys. Res. Lett. 21, 895–898 (1994)CrossRef Wang, Y., Weidner, D.J.: Thermoelasticity of CaSiO3 perovskite and implications for the lower mantle. Geophys. Res. Lett. 21, 895–898 (1994)CrossRef
453.
Zurück zum Zitat Williams, D.W., Kennedy, G.C.: Melting curve of diopside to 50 kilobars. J. Geophys. Res. 74, 4359–4366 (1969)CrossRef Williams, D.W., Kennedy, G.C.: Melting curve of diopside to 50 kilobars. J. Geophys. Res. 74, 4359–4366 (1969)CrossRef
464.
Zurück zum Zitat Yamada, H., Takahashi, E.: Subsolidus phase relations between coexisting garnet and two pyroxenes at 50 to 100 kbar in the system CaO–MgO–Al2O3–SiO2. In: Kornprobst, J. (ed.) Kimberlites II: The Mantle and Crust-Mantle Relationships, pp. 247–255. Elsevier, Amsterdam (1984) Yamada, H., Takahashi, E.: Subsolidus phase relations between coexisting garnet and two pyroxenes at 50 to 100 kbar in the system CaO–MgO–Al2O3–SiO2. In: Kornprobst, J. (ed.) Kimberlites II: The Mantle and Crust-Mantle Relationships, pp. 247–255. Elsevier, Amsterdam (1984)
467.
Zurück zum Zitat Yang, H.-Y.: Crystallization of iron-free pigeonite in the system anorthite-diopside-enstatite-silica at atmospheric pressure. Am. J. Sci. 273, 488–497 (1973)CrossRef Yang, H.-Y.: Crystallization of iron-free pigeonite in the system anorthite-diopside-enstatite-silica at atmospheric pressure. Am. J. Sci. 273, 488–497 (1973)CrossRef
468.
Zurück zum Zitat Yang, H.-Y., Foster, W.R.: Stability of iron-free pigeonite at atmospheric pressure. Am. Mineral. 57, 1232–1241 (1972) Yang, H.-Y., Foster, W.R.: Stability of iron-free pigeonite at atmospheric pressure. Am. Mineral. 57, 1232–1241 (1972)
Metadaten
Titel
System CaO–MgO–SiO2
verfasst von
Professor Tibor Gasparik
Copyright-Jahr
2014
Verlag
Springer New York
DOI
https://doi.org/10.1007/978-1-4614-5776-3_4