Crystal chemistry and significance of cation ordering in Mg-Al rich spinels from high-grade hornfels (Predazzo-Monzoni, NE Italy)

Two Mg-Al spinels (FAS1 and FAS2) in high-grade hornfels from the Teal de M ason skarn (Predazzo Monzoni, NE Italy) were investigated by means of singl e crystal X-ray diffraction and electron microprobe analysis in order to ev aluate the last intra-crystalline closure temperature. The evidence provided by crystal chemical data from the investigated spinel s, compared with that for two other spinels from a websterite dyke and a ch lorite schist (TS2 and SP78a, respectively) with similar chemical character istics, yielded a new empirical geothermometer. This allowed estimation of intra-crystalline temperatures as low as c. 400 degrees C and indicates tha t the closure temperature of FAS1 and FAS2 is c. 500 degrees C, i.e. 150-20 0 degrees C lower than the spinel crystallisation temperature.