C. Cipriani et al., RODOLICOITE AND GRATTAROLAITE, 2 NEW PHOSPHATE MINERALS FROM SANTA-BARBARA MINE, ITALY, European journal of mineralogy, 9(5), 1997, pp. 1101-1106
Grattarolaite and rodolicoite, two new anhydrous iron phosphates, were
found at Santa Barbara lignite mine as reddish-brown nodules. They oc
cur as small crystallites (< 1000 Angstrom), associated in fine-scale
intergrowth that prevent the measurement of physical properties. Gratt
arolaite is trigonal, with space group R3m; rodolicoite is also trigon
al, but with space group P3(1)21. Cell dimensions, calculated from X-r
ay powder patterns, are: grattarolaite a = 7.994(4), c = 6.855(4) Angs
trom, V = 379.4 Angstrom(3), Z = 3; rodolicoite a = 5.048(3), c = 11.2
15(8) Angstrom, V = 247.5 Angstrom(3), Z = 3. The chemical data, obtai
ned by transmission electron microscope microanalysis, give the compos
ition Fe2.99P1.01O7.00 for grattarolaite and Fe1.04P0.96O4.00 for rodo
licoite. Infrared spectroscopy and thermal analysis confirm the anhydr
ous nature of both minerals.