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Zaisho—a pallasite containing pyroxene and phosphoran olivine

Published online by Cambridge University Press:  05 July 2018

Peter R. Buseck  and
Jim Clark
Peter R. Buseck
Affiliation:
Departments of Chemistry, Arizona State University, Tempe, Arizona 85287, USA
Jim Clark
Affiliation:
Departments of Geology, Arizona State University, Tempe, Arizona 85287, USA
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Abstract

The Zaisho meteorite, one of only four known pallasite falls, contains pyroxene, which is rare in pallasites, and it is only the fourth meteorite known to contain phosphoran olivine. Except for a recent report by Goodrich (1984) such olivine appears to be restricted to pallasites, and to those containing the rare Mg phosphate, farringtonite. It is unique among olivines in having P in tetrahedral sites and having vacancies, for charge balance, in octahedral sites. Zaisho also contains stanfieldite and a phosphate having a composition between that of stanfieldite and farringtonite. Its metallographic cooling rate is similar to that of many other pallasites, but its average olivine composition, Fa18.3, places it in a small group with more Fe-rich olivines than most pallasites.

Type
Research Article
Information
Mineralogical Magazine , Volume 48 , Issue 347 , June 1984 , pp. 229 - 235
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1984

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References

Bradley, R. S., Engel, P., and Munro, D. C. (1966) Mineral. Mag. 35, 742–55.Google Scholar
Bunch, T. E., and Keil, K. (1971) Am. Mineral. 56, 146–57.Google Scholar
Buseck, P. R. (1977) Geochim. Cosmochim. Ada. 41, 711–40.CrossRefGoogle Scholar
Buseck, P. R. and Goldstein, J. I. (1969) Geol. Soc. Am. Bull. 80, 2141–58.CrossRefGoogle Scholar
Buseck, P. R. and Holdsworth, E. (1977) Mineral. Mag. 41, 91–102.CrossRefGoogle Scholar
Buseck, P. R. Self, P. G., Von Dreele, R., and Post, J. (1983) Trans. Am. Geophys. Union. 64, 353.Google Scholar
Dodd, R. T. (1969) Geochim. Cosmochim. Ada. 33, 161–203.CrossRefGoogle Scholar
Eventoff, W., Martin, R., and Peacor, D. R. (1972) Am. Mineral. 57, 45–51.Google Scholar
Fleet, M. E., and MacRae, N. D. (1982) Geol. Soc. Am. Abstr. 14, 489.Google Scholar
Goodrich, C. (1984) Geochim. Cosmochim. Ada (submitted).Google Scholar
Jackson, E. D. (1969) Econ. Geol. Monogr. 4, 41–71.Google Scholar
Koritnig, S. (1965) Geochim. Cosmochim. Ada. 29, 361–71.CrossRefGoogle Scholar
Moore, P. B. (1972) Am. Mineral. 57, 24–35.Google Scholar
Narayan, C, and Goldstein, J. I. (1984) submitted to Geochim. Cosmochim. Ada.Google Scholar
Pellas, P., Perron, C, Crozaz, G., Perelygin, V. P., and Stetsenko, S. G. (1981) Meteoritics. 16, 375.Google Scholar
Quensel, P. (1937) Geol. Foren. Forhandl. 59, 77–96.CrossRefGoogle Scholar
Scott, E. R. D. (1977) Mineral. Mag. 41, 265–72.CrossRefGoogle Scholar
Self, P. and Buseck, P. R. (1983) Proc. 41st Ann. Mtg. Electron Micros. Am . 178–81.CrossRefGoogle Scholar
Shima, M., Okada, A., and Yabuki, H. (1980) Z. Natwforsch. 35a, 64–8.Google Scholar