Barioperovskite, BaTiO3,
a new mineral from the Benitoite Mine, California
Chi Ma & George R. Rossman
Division of Geological
and Planetary Sciences
California Institute of Technology
Pasadena, CA 91125-2500, USA
ABSTRACT
Barioperovskite,
ideally BaTiO3, is a
new member of the perovskite group. It is found as micro- to
nano-crystals in a
host of amorphous material contained within hollow, tubular inclusions
in
benitoite from the Benitoite Mine, San Benito County, California, USA.
The mean chemical composition
determined by electron microprobe analysis is (wt%) BaO 65.46, TiO2
34.57, SiO2 0.89, sum
100.92.
The empirical formula calculated on the basis of 3
O = 3 is Ba0.97Ti0.98Si0.03O3.
Barioperovskite is orthorhombic, Amm2;
a= 3.9874 Å, b= 5.6751
Å, c = 5.6901 Å, V =
128.76
Å3, and Z = 2. The electron back
scattered diffraction pattern is an
excellent match to that of synthetic BaTiO3 with
the Amm2 structure. The strongest
calculated
X-ray powder diffraction lines from the synthetic BaTiO3 data
are [d
in Å, (I), hkl] 4.018
(18) (001), 2.845 (30) (002), 2.830 (100) (111), 2.316(20) (102), 2.312
(23)
(120), 2.009 (28) (022), 1.640 (17) (113), 1.637 (19) (131), 1.633 (18)
(202),
1.415 (15) (222). The mineral is named after its composition, a barium
dominant
member of the perovskite group.
Reflected light photomicrograph of barioperovskite
at the edge of a hollow, 60 micrometer wide tubular inclusion
in benitoite.
Backscattered electron image of the same
barioperovskite in the SEM.
American Mineralogist 93, 154-157