Polylithionite
Brigatti M F, Mottana A, Malferrari D, Cibin G
American Mineralogist 92 (2007) 1395-1400
Crystal structure and chemical composition of Li-, Fe-, and Mn-rich micas
Locality: Mokrusha mine, Yuzhakova village, Murzinka region, Russia
Sample: Mokrusha
_database_code_amcsd 0004417
5.297 9.133 10.168 90 100.78 90 C2
atom      x      y     z occ Uiso U(1,1) U(2,2) U(3,3) U(1,2) U(1,3) U(2,3)
SiT1  .0754  .1693 .2296 .83 .013   .009   .010   .023   .004   .006   .001
AlT1  .0754  .1693 .2296 .17 .013   .009   .010   .023   .004   .006   .001
SiT11 .5859  .3332 .2291 .83 .011   .013   .008   .011   .003      0   .002
AlT11 .5859  .3332 .2291 .17 .011   .013   .008   .011   .003      0   .002
LiM1      0  .9920    .5 .66 .015   .011   .010   .025      0   .005      0
FeM1      0  .9920    .5 .17 .015   .011   .010   .025      0   .005      0
MnM1      0  .9920    .5 .16 .015   .011   .010   .025      0   .005      0
MgM1      0  .9920    .5 .01 .015   .011   .010   .025      0   .005      0
AlM2      0  .3226    .5     .014   .005   .009   .028      0   .006      0
LiM3     .5  .1620    .5 .66 .009   .008   .008   .008      0  -.003      0
FeM3     .5  .1620    .5 .19 .009   .008   .008   .008      0  -.003      0
MgM3     .5  .1620    .5 .15 .009   .008   .008   .008      0  -.003      0
KA        0  .5010     0 .94 .029   .028   .023   .035      0   .003      0
NaA       0  .5010     0 .04 .029   .028   .023   .035      0   .003      0
CaA       0  .5010     0 .01 .029   .028   .023   .035      0   .003      0
O1    .0301 1.0026 .1717     .023   .023   .018   .025   .005      0  -.011
O2    .3206  .2370 .1697     .027   .020   .037   .023  -.006   .005  -.008
O22   .8197  .2635 .1633     .021   .019   .023   .023   .007   .010  -.003
O3    .1203  .1770 .3937     .017   .018   .021   .010   .009  -.001  -.002
O33   .6602  .3288 .3931     .021   .027   .008   .028   .010   .004   .002
OH4   .1116  .4749 .4001 .05 .019   .019   .017   .021  -.005   .002  -.001
F4    .1116  .4749 .4001 .95 .019   .019   .017   .021  -.005   .002  -.001