The eudialyte group: a review

Authors

  • Ole Johnsen Geological Museum, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Copenhagen K, Denmark
  • Joel D. Grice Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario, K1P 6P4 Canada
  • Robert A. Gault Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario, K1P 6P4 Canada

DOI:

https://doi.org/10.34194/ggub.v190.5174

Abstract

The eudialyte group of complex Na, Ca, Zr silicates encompasses a wide range of compositions in which all the main elements Si, Zr, Ca, Fe and Na vary, and many relatively minor elements such as Mn, REE, Sr Nb, K, Y and Ti are present. For most members of the group the empirical formula is Na15[M(1)]6[M(2)]3Zr3[M(3)](Si25O73)(O,OH,H2O)3(Cl,F,OH)2 and the best method of formula calculation is on the basis of 29 (Si, Al, Zr Ti, Hf, Nb, W, Ta) apfu (Z = 3), which are the elements assigned to the Zr, M(3) and all Si sites in the structure. The commonest substitutions are found with the solid solution series eudialyte sensu stricto (enriched in Si, Ca, Fe and Cl) and kentbrooksite (enriched in Nb, REE, Mn and F), but recent studies show that the series extends beyond kentbrooksite to an exceptionally Ca-deficient eudialyte now named oneillite. Most eudialytes are trigonal R3m or R3m but oneillite is R3. Additional members of the group are khomyakovite and manganokhomyakovite.

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Published

2001-12-21

How to Cite

Johnsen, O. ., Grice, J. D. ., & Gault, R. A. . (2001). The eudialyte group: a review. Geology of Greenland Survey Bulletin, 190, 65–72. https://doi.org/10.34194/ggub.v190.5174