Sodic-ferripedrizite, ideally Na(LiNa)(Fe23+Mg2Li)Si8O22(OH)(2), is the second new amphibole end-member found in episyenites formed after cordierite-bearing porphyritic granites in the East Pedriza Massif (Central System, Spain). It is green, vitreous, translucent, non-fluorescent and brittle, and has gray streak, H(Mohs) = 6, splintery fracture, perfect {110} cleavage, D-meas = 3.15, D-calc = 3.15 g/ cm(3). In plane-polarized light, sodic-ferripedrizite is strongly pleochroic, X = green blue, Y = blue green, Z = yellow green (X> Y> Z); Y = b, X <^> c = 4 degrees, Z <^> c = -8 degrees. It is biaxial positive: alpha = 1.694 (1), beta = 1.698(1), and gamma = 1.702(1); 2V(z) = 83(2)degrees and 2V(Zcalc) = 85(3)degrees, dispersion r > v. Sodic-ferripedrizite is monoclinic. space group C2/m, an = 9.536(1), b = 17.789(1), c = 5.277(1) Angstrom, beta = 102.53 degrees, V = 873.8(1) Angstrom(3). The five strongest Lines in the X-ray powder-diffraction pattern [d in Angstrom[I] (hkl) are 3.397[3](131), 3.056[10](310), 2.749[5](330), 2.699[6](151), and 1.639[4](461). Analysis by electron microprobe and flame photometry gave an average chemical formula of <^>(Na0.70K0.03) (B)(Li1.34Na Ca-0.58(0.08)) (Mg1.75Fe1.653+Li0.88Fe0.322+Al0.21Ti0.11Mn0.072+Zn0.01)Si8.00O22(OH1.35F0.65). Structure refinement of one crystal of pedrizite and of another crystal with higher clinoholmquistite component, both of which were also analyzed by ion microprobe for light and volatile elements, allowed us to assess Li partitioning among the B- and C-group sites and the active crystal-chemical mechanisms; Li is ordered at the [6+2]-coordinated position in the M4 cavity and at the M3 site. Thus, sodic-ferripedrizite encompasses the different site-preferences and crystal-chemical mechanisms observed for Li in amphiboles of the Mg-Fe-Mn-Li group (clinoholmquistite series) and the Na-Ca group (leakeite series). These data and other recent results on synthetic amphiboles suggest that miscibility between the two groups of B-cations is far more extensive than previously expected.
Sodic-ferripedrizite, a new monoclinic amphibole bridging the magnesium-iron-manganese-lithium and the sodium-calcium groups
Oberti R;Ottolini L;
2000
Abstract
Sodic-ferripedrizite, ideally Na(LiNa)(Fe23+Mg2Li)Si8O22(OH)(2), is the second new amphibole end-member found in episyenites formed after cordierite-bearing porphyritic granites in the East Pedriza Massif (Central System, Spain). It is green, vitreous, translucent, non-fluorescent and brittle, and has gray streak, H(Mohs) = 6, splintery fracture, perfect {110} cleavage, D-meas = 3.15, D-calc = 3.15 g/ cm(3). In plane-polarized light, sodic-ferripedrizite is strongly pleochroic, X = green blue, Y = blue green, Z = yellow green (X> Y> Z); Y = b, X <^> c = 4 degrees, Z <^> c = -8 degrees. It is biaxial positive: alpha = 1.694 (1), beta = 1.698(1), and gamma = 1.702(1); 2V(z) = 83(2)degrees and 2V(Zcalc) = 85(3)degrees, dispersion r > v. Sodic-ferripedrizite is monoclinic. space group C2/m, an = 9.536(1), b = 17.789(1), c = 5.277(1) Angstrom, beta = 102.53 degrees, V = 873.8(1) Angstrom(3). The five strongest Lines in the X-ray powder-diffraction pattern [d in Angstrom[I] (hkl) are 3.397[3](131), 3.056[10](310), 2.749[5](330), 2.699[6](151), and 1.639[4](461). Analysis by electron microprobe and flame photometry gave an average chemical formula of <^>(Na0.70K0.03) (B)(Li1.34Na Ca-0.58(0.08)) (Mg1.75Fe1.653+Li0.88Fe0.322+Al0.21Ti0.11Mn0.072+Zn0.01)Si8.00O22(OH1.35F0.65). Structure refinement of one crystal of pedrizite and of another crystal with higher clinoholmquistite component, both of which were also analyzed by ion microprobe for light and volatile elements, allowed us to assess Li partitioning among the B- and C-group sites and the active crystal-chemical mechanisms; Li is ordered at the [6+2]-coordinated position in the M4 cavity and at the M3 site. Thus, sodic-ferripedrizite encompasses the different site-preferences and crystal-chemical mechanisms observed for Li in amphiboles of the Mg-Fe-Mn-Li group (clinoholmquistite series) and the Na-Ca group (leakeite series). These data and other recent results on synthetic amphiboles suggest that miscibility between the two groups of B-cations is far more extensive than previously expected.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
