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Manganese thermometer for mantle peridotites

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Abstract

The temperature dependence of the Mn-Mg distribution between garnet and clinopyroxene, originally proposed by Carswell, was confirmed by Shimizu and Allègre (1978) using ion microprobe and electron microprobe data. High precision electron microprobe analyses of a larger set of 52 Iherzolites from S. Africa and Malaita, Solomon Islands show considerable scatter in the temperature dependence of this distribution, and correlation with the CaO content of the garnet is indicated. A new distribution coefficient is based on the reaction:

$$\begin{gathered} \operatorname{Mn} _{\text{2}} \operatorname{Si} _2 \operatorname{O} _6 {\text{ + }}\operatorname{CaAl} _{2/3} \operatorname{SiO} _4 {\text{ + }}\operatorname{MgAl} _{2/3} \operatorname{SiO} _4 \hfill \\ {\text{Mn - pyroxene grossular pyrope}} \hfill \\ {\text{ }} \rightleftharpoons \operatorname{CaMgSi} _2 \operatorname{O} _6 {\text{ + }}2\operatorname{MnAl} _{2/3} \operatorname{SiO} _4 \hfill \\ {\text{ diopside spessartine}} \hfill \\ \end{gathered} $$

It was calibrated against temperature determined from two independent thermometers (Wells pyroxene and O'Neill-Wood garnet-olivine) for Iherzolitic assemblages, and shown to to be sensitive to within + 50 °C for most specimens in the range 900 °– 1,300 ° C. This distribution coefficient appears independent of pressure within the uncertainty of the available data, and has the potential to be a third independent thermometer for use in garnet Iherzolites and possibly eclogites.

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References

  • Akella, J., Boyd, F.R.: Petrogenetic grid for garnet peridotite. Carnegie Inst. Washington Yearb. 73, 269–273 (1974)

    Google Scholar 

  • Akimoto, S., Syono, Y.: High pressure transformations in MnSiO3. Am. Mineral 57, 76–84 (1972)

    Google Scholar 

  • Bishop, F.C., Smith, J.V., Dawson, J.B.: Na, K, P, and Ti in garnet, pyroxene and olivine from peridotite and eclogite xenoliths from African kimberlites. Lithos 11, 155–174 (1978)

    Google Scholar 

  • Bloomer, A.G., Nixon, P.H.: The geology of the Letseng-la-terae kimberlite pipes. In: Lesotho kimberlites (P.H. Nixon, ed.), pp. 20–33. Maseru, Lesotho: Lesotho National Development Corporation 1973

    Google Scholar 

  • Boyd, F.R., Finger, L.W.: Homogeneity of minerals in mantle rocks from Lesatho. Carnegie Inst. Washington Yearb. 74, 519–525 (1975)

    Google Scholar 

  • Boyd, F.R., Nixon, P.H.: Ultramafic xenoliths and xenocrysts from the Kimberley pipes, south Africa. Unpublished technical report issued by F.R. Boyd, Geophysical Laboratory, Washington, D.C., U.S.A. 1976

    Google Scholar 

  • Carswell, D.A.: Comparative equilibration temperatures and pressures of garnet Iherzolites in Norwegian gneisses and in kimberlite. Lithos 7, 113–121 (1974)

    Google Scholar 

  • Charlu, T.V., Newton, R.C., Kleppa, O.J.: Enthalpies of formation at 970 ° K of compounds in the system MgO-Al2O3-SiO2 from high temperature solution calorimetry. Geochim. Cosmochim. Acta 39, 1487–1497 (1975)

    Google Scholar 

  • Davis, B.T.C., Boyd, F.R.: The join Mg2Si2O6-CaMgSi2O6 at 30 kbar pressure and its application to kimberlite. J. Geophys. Res. 71, 3567–3576 (1966)

    Google Scholar 

  • Delaney, J.S., Smith, J.V., Nixon, P.H.: Model for upper mantle below Malaita, Solomon Islands. Contrib. Mineral. Petrol. 70, 209–218 (1979)

    Google Scholar 

  • Finnerty, T.A.: Exchange of Mn, Ca, Mg, and Al between synthetic garnet, orthopyroxene, clinopyroxene and olivine. Carnegie Inst. Washington Yearb. 76, 572–579 (1977)

    Google Scholar 

  • Holst, N.B. Jr.: The use of thermodynamic excess functions in the Nernst distribution law. Am. Mineral. 63, 83–86 (1978)

    Google Scholar 

  • Jawardena, D.E., De S., Carswell, D.A.: The geochemistry of ‘charnockites’ and their constituent ferromagnesian minerals from the Precambrian of south-east Sri Lanka (Ceylon). Mineral. Mag. 40, 541–554 (1976)

    Google Scholar 

  • Lindstrom, D.J., Weill, D.F.: Partitioning of transition metals between diopside and coexisting silicate liquids — 1. Ni, Co, Mn. Geochim. Cosmochim. Acta 42, 817–833 (1978)

    Google Scholar 

  • Navrotsky, A., Coons, W.E.: Thermochemistry of some pyroxenes and related compounds. Geochim. Cosmochim. Acta 40, 1281–1288 (1976)

    Google Scholar 

  • Nixon, P.H., Boyd, F.R.: Petrogenesis of the granular and sheared ultrabasic nodule suite in kimberlites. In: Lesotho komberlites (P.H. Nixon, ed.), pp. 48–57. Maseru, Lesotho: Lesotho National Development Corporation 1973a

    Google Scholar 

  • Nixon, P.H., Boyd, F.R.: The liqhobong intrusions and kimberlite olivine composition. In: Lesotho kimberlites (P.H. Nixon, ed.), pp. 141–149. Maseru, Lesotho: Lesotho National Development Corporation 1973b

    Google Scholar 

  • Nixon, P.H., Boyd, F.R.: Garnet bearing ultrabasic and discrete nodule suites from Malaita, Somomon Islands, S.W. Pacific, and their bearing on oceanic mantle composition and geotherm. Proc. 2nd Int. Kimperlite Conf., vol. 2. The Mantle Sample: Inclusions in kimperlites and other volcanics (F.R. Boyd and H.O.A. Meyer, eds.), pp. 400–423. Washington, D.C.: American Geophysical Union 1979

    Google Scholar 

  • O'Neill, H., Wood, B.J.: An experimental study of Fe-Mg partitioning between garnet and olivine and its calibration as a geothermometer 1979

  • Råheim, A., Green, D.H.: Experimental determination of the temperature and pressure dependence of the Fe-Mg partition coefficient for coexisting garnet and clinopyroxene. Contrib. Mineral. Petrol. 48, 179–203 (1974)

    Google Scholar 

  • Robie, R.A., Hemingway, B.S., Fisher, J.R.: Thermodynamic properties of minerals and related substances at 298.15 ° K and 1 bar (105 Pa) pressure and at higher temperatures. U.S. Geol. Surv. Bull. 1452 (1978)

  • Shearer, J.A.: Thermochemistry of the garnets and some related compounds. University Chicago: Ph.D. Thesis 1973

  • Shimizu, N., Allègre, C.J.: Geochemistry of transition elements in garnet Iherzolite nodules in kimberlites. Contrib. Mineral. Petrol. 67, 41–51 (1978)

    Google Scholar 

  • Shimizu, N., Semet, M.P., Allègre, C.J.: Geochemical applications of quantitative ion-microprobe analysis. Geochim. Cosmochim. Acta 42, 1321–1335 (1978)

    Google Scholar 

  • Smith, J.V., Stephenson, D.A., Howie, R.A., Hey, M.H.: Relations between cell dimensions, chemical compositions and site preference of orthopyroxene. Mineral. Mag. 37, 90–115 (1969)

    Google Scholar 

  • Steele, I., Hutcheon, I.: Ion probe analysis of natural olivine: secondary ion intensity variation and systematics for a simple binary silicate. San Antonio, Texas: Microbeam Analysis Society, abstr. for meeting 1979

  • Wells, P.: Pyroxene thermometry in simple and complex systems. Contrib. Mineral. Petrol. 62, 129–139 (1977)

    Google Scholar 

  • Wood, B.J.: The partitioning of iron and magnesium between garnet and clinopyroxene. Carnegie Inst. Washington Yearb. 75, 571–575 (1976)

    Google Scholar 

  • Wood, B.J., Banno, S.: Garnet-orthopyroxene and orthopyroxeneclinopyroxene relations in simple and complex systems. Contrib. Mineral. Petrol. 42, 109–124 (1974)

    Google Scholar 

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Delaney, J.S., Smith, J.V., Dawson, J.B. et al. Manganese thermometer for mantle peridotites. Contrib. Mineral and Petrol. 71, 157–169 (1979). https://doi.org/10.1007/BF00375432

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