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American Mineralogist; February 2002; v. 87; no. 2-3; p. 355-358
© 2002 Mineralogical Society of America
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NEW MINERAL NAMES*

John L. Jambor1 and Andrew C. Roberts2

1 Department of Earth and Ocean Sciences, University of British Columbia, Vancouver, British Columbia, V6T 1Z4, Canada
2 Geological Survey of Canada, 601 Booth Street, Ottawa K1A 0E8, Canada

The first 20% of the full text of this article appears below.

Bigcreekite*
L.C. Basciano, L.A. Groat, A.C. Roberts, R.A. Gault, G.E. Dunning, R.E. Walstrom (2001) Bigcreekite: a new barium silicate mineral species from Fresno County, California. Can. Mineral., 39, 761–768.

Four listed electron microprobe analyses, with high totals because of water loss, average Na2O 0.11, CaO 0.03, SrO 0.02, BaO 48.88, SiO2 38.16, H2O (calc.) 22.94, sum 110.14 wt%, corresponding to Ba1.00Na0.01Si2.00O5•4H2O, ideally BaSi2O5•4H2O. Occurs as white to colorless, millimeters-long, subhedral tabular grains, elongate [100]. Brittle, white streak, vitreous to pearly luster, H = 2–3, perfect {010} and {001} cleavages, uneven fracture, nonfluorescent, Dmeas = 2.66, Dcalc = 2.76 g/cm3 for Z = 4. Optically biaxial positive, {alpha} = 1.537(2), ß = 1.538(2), {gamma} = 1.541(2), 2Vmeas = 59.2(5), 2Vcalc = 60°, moderate dispersion r < v, nonpleochroic, orientation X = b, Y = a, Z = c. Single-crystal X-ray structure study (R = 0.035) indicated orthorhombic symmetry, space group Pnma, a = 5.038(6), b = 9.024(3), c = 18.321(6) Å as refined from a Debye–Scherrer powder pattern (114 mm, CuK{alpha} radiation) with strongest lines of 5.068 (100,013), 4.054(85,022), 2.974(45,031), 2.706 (60,124), 2.327(40,035), and 2.257(75,126).

The mineral occurs within fractures, <0.5 mm wide, transverse to sanbornite-quartz gneiss at the Esquire no. 7 claim along Big Creek, Fresno County, California. The new mineral name is for the type locality. The mineral also occurs as a fracture fill in lenses of barium silicates, including sanbornite, at Trumbull Peak, Mariposa County, California. Type material is in the M.Y. Williams Museum at the University of British Columbia, Vancouver, Canada. J.L.J.

Clearcreekite*
A.C. Roberts, L.A. Groat, M. Raudsepp, T.S. Ercit, R.C. Erd, E.A. Moffat, J.A.R. Stirling (2001) Clearcreekite, a new polymorph of Hg31+(CO3)(OH)•2H2O, from the Clear Creek claim, . . . [Full Text of this Article]




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