J. Schluter et al., GORDAITE, NAZN4(SO4)(OH)(6)CL-CENTER-DOT-6H(2)O, A NEW MINERAL FROM THE SAN-FRANCISCO MINE, ANTOFAGASTA, CHILE, Neues Jahrbuch fur Mineralogie Monatshefte, (4), 1997, pp. 155-162
Gordaite, a new hydrous sodium zinc hydroxy-chlorosulfate, ideally NaZ
n4(SO4)(OH)(6)Cl . 6H(2)O, Z = 2, is trigonal, space group P (3) over
bar, with a = 8.3556(3) Angstrom, c = 13.025(1) Angstrom, from single
crystal studies. The strongest reflections in the X-ray powder diffrac
tion data are (d(meas.),I,hkl) 12.950(100) (001), 6.501(23) (002) and
4.339(15) (003). The mineral occurs at the San Francisco Mine, Sierra
Gorda, northeast of Antofagasta, Chile. It forms masses of white to co
lorless platy crystals. Electron microprobe and CHN analyses yielded N
a2O 9.15, ZnO 52.85, SO3 15.33, Cl 6.46, H2O 12.33. Gordaite is probab
ly identical with an unnamed mineral (ICDD-PDF 41-1421) which has been
found on sulfide samples from the Juan de Fuca Ridge, NE Pacific.