
Vol. 44, pp. 105-115 (2006)
Johnsenite-(ce): a new member of the eudialyte group from Mont Saint-Hilaire, Quebec, Canada
Joel D. Grice and Robert A. Gault

Vol. 44, pp. 105-115 (2006)
ABSTRACT
Johnsenite-(Ce), ideally Na12(Ce,La,Sr,Ca,M)3Ca6Mn3Zr3W(Si25O73)(CO3)(OH,Cl)2, is a new member of the eudialyte group from Mont Saint-Hilaire, Quebec, and is the W analogue of zirsilite-(Ce). It occurs as deeply etched, skeletal crystals to 4 mm and aggregates of crystals to 1 cm. Associated minerals include, albite, calcite, pectolite, aegirine, fluorapophyllite, zirsilite-(Ce), a burbankite-group phase, dawsonite, rhodochrosite, epididymite, galena, molybdenite, pyrite, pyrrhotite, quartz, an amphibole-group mineral, sphalerite, stillwellite-(Ce), titanite, cerite-(Ce), tuperssuatsiaite, steacyite, catapleiite, zakharovite, natrolite and microcline. It is transparent to translucent with a vitreous luster and white streak. It is brittle with a Mohs hardness of 5 - 6. It has no discernable cleavage or parting and an uneven fracture. It is uniaxiail negative with v 1.648(1) and ' 1.637(1). It is trigonal, space group, R3m, a 14.237(3) and c 30.03(1) Å, V 5271(2) Å3M, Z = 3.
The eight strongest X-ray powder-diffraction lines, measured for johnsenite-(Ce) [d in Å (l)(hkl)] are:
The infrared spectrum of johnsenite-(Ce) is given. An average result of eight electron-microprobe analyses, including three on the grain used for the structure determination, gave:
Concentrations of CO2 and H2O were calculated by stoichiometry based on results from the crystal-structure analysis. The empirical formula of johnsenite-(Ce), based on 29 (Si4+, Zr4+, Ti4+, Hf4+, Nb5+, W6+) cations and 1 (CO3) as determined in the crystal-structure analysis, is:
Na11.74 ([Ce0.64La0.33Dy0.03]S1.00Sr0.54Ca0.51Y0.22K0.19)S2.46
(Ca5.06[Pr0.24Nd0.18Gd0.06Sm0.02]S0.50Mn0.44)S6(Mn2.22Fe0.78)S3
(Zr2.71Ti0.32Hf0.01)S3.04(W0.78Nb0.21)S0.99Si24.97O73(CO3)(OH,Cl0.75)S2.
Dmeas. = 3.24(3) g/cm3; Dcalc. = 3.23 g/cm3.
The structure consists of four layers. The layering is disctinctly polar, as indicated by the X-ray-diffraction intensity statistics, leyer composition and electrostatic potential of individual crystals. The new species is named after Ole Johnsen, of the Geological Museum, University of Copenhagen, Denmark.
Keywords: johnsenite-(Ce), eudialyte, new mineral species, crystal structure, Mont Saint-Hilaire, Quebec.

© 2006 The Canadian Mineralogist