Tremolite Oberti R, Camara F, Ottolini L American Mineralogist 90 (2005) 732-736 Clinoholmquistite discredited: The new amphibole end-member fluoro-sodic-pedrizite sample from Tastyg spodumene deposit, Tuva, Siberia, Russia _database_code_amcsd 0003771 9.848 18.049 5.279 90 104.73 90 C2/m atom x y z occ Biso B(1,1) B(2,2) B(3,3) B(1,2) B(1,3) B(2,3) NaA2 0 .483 0 .031 2.0 .0088 .0016 .0280 0 .0119 0 KA2 0 .483 0 .019 2.0 .0088 .0016 .0280 0 .0119 0 NaAm .040 .5 .093 .049 .8 .0002 .0013 .0073 0 .0010 0 KAm .040 .5 .093 .031 .8 .0002 .0013 .0073 0 .0010 0 Mg1 0 .0880 .5 .98 .56 .0015 .0004 .0061 0 .0008 0 Fe1 0 .0880 .5 .04 .56 .0015 .0004 .0061 0 .0008 0 Mg2 0 .1770 0 .975 .53 .0014 .0004 .0058 0 .0008 0 Fe2 0 .1770 0 .010 .53 .0014 .0004 .0058 0 .0008 0 Mn2 0 .1770 0 .005 .53 .0014 .0004 .0058 0 .0008 0 Ti2 0 .1770 0 .005 .53 .0014 .0004 .0058 0 .0008 0 Zn2 0 .1770 0 .005 .53 .0014 .0004 .0058 0 .0008 0 Mg3 0 0 0 .84 .59 .0016 .0004 .0059 0 .0005 0 Al3 0 0 0 .08 .59 .0016 .0004 .0059 0 .0005 0 Fe3 0 0 0 .08 .59 .0016 .0004 .0059 0 .0005 0 Ca4 0 .2778 .5 .925 .79 .0024 .0005 .0097 0 .0028 0 Na4 0 .2778 .5 .075 .79 .0024 .0005 .0097 0 .0028 0 Si1 .2802 .0842 .2974 .991 .44 .0011 .0003 .0052 -.0001 .0005 -.0001 Al1 .2802 .0842 .2974 .008 .44 .0011 .0003 .0052 -.0001 .0005 -.0001 B1 .2802 .0842 .2974 .001 .44 .0011 .0003 .0052 -.0001 .0005 -.0001 Si2 .2881 .1712 .8047 .991 .45 .0011 .0003 .0050 -.0001 .0006 .0000 Al2 .2881 .1712 .8047 .008 .45 .0011 .0003 .0050 -.0001 .0006 .0000 B2 .2881 .1712 .8047 .001 .45 .0011 .0003 .0050 -.0001 .0006 .0000 O1 .1117 .0859 .2179 .55 .0013 .0004 .0059 .0000 .0003 .0000 O2 .1186 .1709 .7250 .59 .0012 .0005 .0063 -.0001 .0004 -.0002 O3 .1087 0 .7155 .835 .76 .0020 .0006 .0078 0 .0010 0 F .1087 0 .7155 .165 .76 .0020 .0006 .0078 0 .0010 0 O4 .3647 .2480 .7928 .76 .0023 .0004 .0085 -.0004 .0012 -.0001 O5 .3465 .1340 .0996 .74 .0019 .0006 .0069 .0000 .0008 .0007 O6 .3437 .1184 .5902 .68 .0016 .0006 .0060 .0000 .0008 -.0005 O7 .3374 0 .2921 .79 .0021 .0004 .0105 0 .0008 0 H .190 0 .759 .835 .2