Banfield J F, Bailey S W
American Mineralogist 81 (1996) 79-91
Formation of regularly interstatified serpentine-chlorite minerals by
tetrahedral inversion in long-period serpentine polytypes
_database_code_amcsd 0001773
5.323 9.214 21.381 90 90.00 90 Cm
atom x y z
Mg 0 0 0
Mg .0000 .3333 .0000
O .3333 0 .0493
O .3333 .3333 .0513
Si .3333 .3333 .1278
O .8333 0 .1554
O .0833 .2500 .1554
O .6667 0 .2865
O .6667 .3333 .2865
Mg .0000 0 .3333
Mg .0000 .3333 .3333
O .0000 0 .3801
O .3333 .3333 .3801
O .1667 0 .5112
O .4167 .2500 .5112
Si .6667 .3333 .5388
O .6667 0 .6173
O .6667 .3333 .6153
Mg .0000 0 .6667
Mg .0000 .3333 .6667
O .3333 0 .7135
O .3333 .3333 .7135
O .1667 0 .8446
O .4167 .2500 .8446
Si .6667 .3333 .8722
O .6667 0 .9507
O .6667 .3333 .9487
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