Page 84 - A Practical Introduction to Optical Mineralogy
P. 84

SILICATE  MINERALS                                                         FELDSPAR  GROUP
                         Alkali feldspars                                               • h lh~tt'htse-low albite series   Or,oo-85   orthoclase
                         There  is  a  continuous  series  from  K-feldspar  (KA1Si 3 0 8 )  to  albite        Or 85-20   orthoclase cryptoperthites
                         (NaA1Si 30 8 )  for  high  and low alkali feldspars.                                  Or20-o     low  albite

             Sanidine-high albite series   Ab 0 - Ab 63   sanidine                       IJ, •m·lln  low albite series   Or,oo-n   microcline
                                                anorthoclase                                                              microcline cryptoperthites
                                    Ab 63 - Ab 90                                                              Or •2-zo
                                                high  albite                                                              low  albite
                                    Ab. 0- Ab 100                                                              Or zo- o

                                                                                                                    Orthoclase                  Microcline
                                       High sanidine       c       Low sanidinc                                                         c
                             'I                             I                                                 c                         I
                             I                              I                                              13  I   I                    I
                             I                              l                                                 I                         I
                              I   lXII                      I   00 1                                        I   I
                                                                                                            I   I                       I




                                                                   - -b ='I


                                                                                                                                 /
                                                                                                                                /
                                                                                                      /
                                                                                                      /                       Cl./
                                                                                                     /
                                                                                                    Cl.


                                                   13
                                                   I
                                                  I
                                                  I
                                              001  /
                                                I











                                                       High albite



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