Ys. Borodaev et al., Rare sulfosalts from Vulcano, Aeolian Islands, Italy. I. Se-bearing kirkiite, Pb-10(Bi,As)(6)(S,Se)(19), CAN MINERAL, 36, 1998, pp. 1105-1114
This note reports the first occurrence of a Se-bearing variety of kirkiite,
a rare lead - bismuth - arsenic sulfosalt, from the deepest part of fumaro
le F11, La Fossa crater, island of Vulcano, Italy. Small crystals of sphale
rite and aggregates of cannizzarite occur sporadically on the kirkiite crys
tals. Optical properties, X-ray powder-diffraction data and the results of
electron-microprobe analyses are compared with those of kirkiite from type
locality as well as of phase A? the synthetic analogue. An electron-microdi
ffraction study revealed the presence of three structural varieties of kirk
iite. The Se content ranges from 0.73 to 1.16 wt%. As and Bi concentrations
vary from 6.49 to 7.98 wt% and from 14.32 to 16.84 wt%, respectively. The
composition field of kirkiite from Vulcano can be described by the formula
Pb-10(As6-xBix)(Sigma 6)(S19-ySey)(Sigma 19), where 2.3 less than or equal
to x less than or equal to 2.8 and 0.3 less than or equal to y less than or
equal to 0.5, which is close to the ideal formula Pb-10(As,Bi)(6)(S,Se)(19
). Kirkiite and its associated minerals at Vulcano crystallized at a high f
ugacity of sulfur and a high temperature (470 degrees C, direct measurement
s). This temperature is in agreement with that known for the synthetic anal
ogue, stable at 400 degrees C.