Feldspar Benna P, Bruno E American Mineralogist 88 (2003) 1532-1541 Single-crystal in situ high-temperature structural investigation of the I-1 - I2/c phase transition in Ca0.2Sr0.8Al2Si2O8 feldspar T = 20 C _database_code_amcsd 0003177 8.361 12.973 14.259 90.79 115.55 90.62 I-1 atom x y z occ Uiso U(1,1) U(2,2) U(3,3) U(1,2) U(1,3) U(2,3) Ca(0) .2694 .0014 .0669 .2 .020 .008 .028 .022 .000 .003 -.011 Sr(0) .2694 .0014 .0669 .8 .020 .008 .028 .022 .000 .003 -.011 Ca(z) .2678 .0072 .5629 .2 .016 .008 .020 .017 .000 .004 -.003 Sr(z) .2678 .0072 .5629 .8 .016 .008 .020 .017 .000 .004 -.003 SiT1(00) .0070 .1698 .1072 .010 .009 .011 .009 -.003 .005 .000 AlT1(0z) .0029 .1737 .6154 .009 .010 .010 .009 -.002 .005 .000 AlT1(m0) .0022 .8194 .1176 .009 .010 .010 .009 .001 .005 .000 SiT1(mz) .0068 .8222 .6095 .009 .009 .011 .008 .002 .004 .001 AlT2(00) .6919 .1185 .1669 .009 .008 .008 .010 .000 .003 .000 SiT2(0z) .6830 .1112 .6681 .009 .008 .008 .011 -.001 .004 .000 SiT2(m0) .6844 .8852 .1754 .009 .008 .008 .010 .000 .004 .000 AlT2(mz) .6927 .8781 .6724 .008 .008 .008 .010 .000 .004 .000 OA(10) .0064 .1279 .9978 .014 .017 .017 .009 -.003 .007 .000 OA(1z) .9945 .1287 .4966 .013 .014 .016 .010 .002 .008 .002 OA(20) .5884 .9965 .1421 .013 .012 .008 .018 .000 .006 .002 OA(2z) .5874 .9967 .6422 .013 .010 .008 .019 -.001 .006 .002 OB(00) .8251 .1190 .1012 .016 .013 .017 .021 -.004 .011 -.001 OB(0z) .8061 .1194 .6067 .015 .015 .017 .018 -.003 .011 .000 OB(m0) .8100 .8675 .1174 .018 .015 .022 .024 .003 .013 -.003 OB(mz) .8275 .8679 .6087 .016 .014 .020 .018 .005 .011 .002 OC(00) .0148 .2924 .1242 .016 .015 .013 .019 -.006 .007 -.004 OC(0z) .0193 .3047 .6381 .016 .015 .012 .020 -.006 .007 -.003 OC(m0) .0144 .6865 .1229 .015 .014 .011 .019 .003 .006 .001 OC(mz) .0094 .6979 .6119 .015 .013 .012 .018 .002 .005 .000 OD(00) .1857 .1184 .1930 .017 .014 .023 .012 .001 .004 .002 OD(0z) .1979 .1132 .6995 .016 .015 .017 .012 .002 .001 .002 OD(m0) .1991 .8768 .2078 .015 .012 .017 .013 .000 .001 -.001 OD(mz) .1877 .8697 .7000 .018 .015 .021 .015 -.002 .002 -.003