Skip to main content
Log in

Temperature dependence of intersite distribution of Mg and Fe in olivine and the associated change of lattice parameters

  • Published:
Physics and Chemistry of Minerals Aims and scope Submit manuscript

Abstract

The cation distribution of natural and heated ferromagnesian olivine with chemical composition, Fo67Fa33, from metagabbro was examined by X-ray diffraction. Heating and quenching experiments were made by a newly devised apparatus which enables us to obtain very fast quenching speed in comparison with the usual technique. The distribution constants, K D=(Fe+2/Mg) M1/(Fe+2/Mg) M2, of the natural samples were less than 1.07, and those of heat-treated samples were more than 1.15, indicating that cation ordering takes place with temperature. The distribution of Fe+2 and Mg is nearly random at low temperatures, whereas Fe+2 shows a slight but significant preference for a smaller M1 site at high temperatures. The change of the distribution constant was observed on specimens which were heated for a short period of time (6–1,060 s) and quenched within 10 ms. Thus the rate of the cation reordering reaction is a very fast process. The lattice parameters b and c decrease whereas a increases with the increase of distribution constant. The overall effect on unit cell volume is a decrease with the increasing distribution constant, suggesting the presence of significant pressure dependence of the cation distribution towards the ordering of Fe at M1 site in ferromagnesian olivine.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Ando K, Kurokawa H, Oishi Y (1981) Self-diffusion coefficient of oxygen in single-crystal forsterite. J Am Ceram Soc 64:c–30

    Google Scholar 

  • Basso R, Dal Negro A, Della Giusta A (1979) Fe/Mg distribution in the olivine of ultrafemic nodule from Assab (Ethiopia). Neues Jahrb Mineral Monatsh: 197–202

  • Bence AE, Albee AL (1968) Empirical correction factors for the electron microanalysis of silicate and oxide. J Petrol 76:382–403

    Google Scholar 

  • Besancon JR (1981) Rate of cation distribution in orthopyroxene. Am Mineral 66:965–973

    Google Scholar 

  • Birle D, Gibbs GV, Moore PB, Smith JV (1968) Crystal structure of natural olivines. Am Mineral 53:807–824

    Google Scholar 

  • Brown GE, Prewitt CT (1973) High temperature crystal chemistry of hortonolite. Am Mineral 58:577–587

    Google Scholar 

  • Burns RG (1969) Evidence for cation ordering in olivine minerals from crystal field spectra (abstract) Acta Crystallogr A25:559

    Google Scholar 

  • Burns RG (1970) Crystal field spectra and evidence of cation ordering in olivine minerals. Am Mineral 55:1608–1632

    Google Scholar 

  • Bush WR, Hafner SS, Virgo D (1970) Some ordering of iron and magnesium at the octahedrally coordinated sites in a magnesium rich olivine. Nature 227:1339–1341

    Google Scholar 

  • Champness PE (1970) Neucleation and growth of iron oxides in olivines, (Mg,Fe)2SiO4. Mineral Mag 37:790–800

    Google Scholar 

  • Doyle PA, Turner PS (1968) Relativistic Hartree-Fock X-ray scattering factors. Acta Crystallogr A24:390–397

    Google Scholar 

  • Finger WL (1970) Fe/Mg ordering in olivines. Carnegie Inst Washington Yearb 69:302–305

    Google Scholar 

  • Finger WL, Virgo D (1971) Confirmation of Fe/Mg ordering in olivines. Carnegie Inst Washington Yearb 70:221–225

    Google Scholar 

  • Finger WL (1972) A Fortran IV Computer Program for structure factor calculation and least-squares refinement of crystal structures. Geophys Lab, Carnegie Inst Washington, Washington D.C.

    Google Scholar 

  • Francis CA, Ribbe PH (1980) The forsterite-tephroite series I. Crystal structure refinements. Am Mineral 65:1263–1269

    Google Scholar 

  • Fujino K (1980) Crystal chemistry of Mn-Mg-Fe olivine solid solution series. J Mineral Soc Japan 14, Spec Issue 3:135–143 (in Japanese with english abstract)

    Google Scholar 

  • Ganguli J (1977) Crystal chemical aspects of olivine structures. Neues Jahrb Mineral Abh 130:303–318

    Google Scholar 

  • Ghose S, Wan C, Okamura PF, Ohashi H, Weidner JR (1975) Site preference and crystal chemistry of transition metal ions in pyroxenes and olivines. Acta Crystallogr A31, Suppl S 76

  • Ghose S, Wan C, McCallum IS (1976) Fe+2-Mg+2 order in an olivine from the lunar anorthosite 67075 and the significance of cation order in lunar and terrestrial olivines. Indian J Earth Sci 3:1–8

    Google Scholar 

  • Henke K (1965) Beiträge zu Kristallstructuren vom Olivin-typ. Beitr Mineral Petrogr 11:535–558

    Google Scholar 

  • Lumpkin GR, Ribbe PH (1983) Composition, order-disorder and lattice parameters of olivines: Relationship in silicate, germanate, beryllate, phosphate and borate olivines. Am Mineral 68:164–176

    Google Scholar 

  • Lumpkin GR, Ribbe PH, Lumpkin NE (1983) Composition, orderdisorder and lattice parameters of olivines: Determinative methods for Mg-Mn and Mg-Ca silicate olivines. Am Mineral 68:1174–1182

    Google Scholar 

  • Mokeyeva VI, Simonov MA, Belokoneva EL, Makarov ES, Ivanov VI, Rannev NV (1977) X-ray study of details of atomic structure and distribution of magnesium and iron atoms in lunar and terrestrial olivines. Geochem Interna 13:50–57

    Google Scholar 

  • Moor JG, Evans BW (1967) The role of olivine in the crystallization of the Prehistoric Makaopuli Tholeiitic Lava Lake, Hawaii. Contrib Mineral Petrol 15:202–223

    Google Scholar 

  • Nakamura Y, Kushiro I (1970) Compositional relations of coexisting orthopyroxene, pigeonite and augite in a tholeiitic andesite from Hakone Volcano. Contrib Mineral Petrol 26:265–275

    Google Scholar 

  • Shinno I (1974) Mössbauer studies of natural olivines. Mineral J Japan 7:344–358

    Google Scholar 

  • Shinno I (1974) Mössbauer studies of olivine, — the relation between Fe+2 site occupancy numbers TMi and interplanner distances d130 —. Memoirs Geol Soc Japan 11:11–17

    Google Scholar 

  • Shinno I (1980) On the distribution of cation in (Mg, Fe)2SiO4 solid solution. Sci ReptDepart Geol Kyushu Univ 13:217–224 (in Japanese with english abstract)

    Google Scholar 

  • Smyth JR, Hazen RM (1973) The crystal structure of forsterite and hortonolite at several temperature up to 900° C. Am Mineral 58:588–593

    Google Scholar 

  • Virgo D, Hafner SS (1972) Temperature-dependent Mg, Fe distribution in a lunar olivine. Earth Planet Sci Letters 14:305–312

    Google Scholar 

  • Wenk HR, Raymond KN (1973) Four new structure refinements of olivine. Z Kristallogr 137:86–105

    Google Scholar 

  • Yoshizawa H, Nakajima W, Ishizaka K (1966) The Ryoke metamorphic zone of Kinki district, Southern Japan: Accomplishment of a regional geological map. Memoirs Coll Sci Univ Kyoto, Ser B32:437–454

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Aikawa, N., Kumazawa, M. & Tokonami, M. Temperature dependence of intersite distribution of Mg and Fe in olivine and the associated change of lattice parameters. Phys Chem Minerals 12, 1–8 (1985). https://doi.org/10.1007/BF00348738

Download citation

  • Received:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF00348738

Keywords

Navigation