Scapolite
      Sokolova E, Hawthorne F C
      The Canadian Mineralogist 46 (2008) 1527-1554
      The crystal chemistry of the scapolite-group minerals. I. crystal structure and
      long-range order
      Locality: Minden, Canada
      Note: S12
      _database_code_amcsd 0006225

      CELL PARAMETERS:   12.1338  12.1338   7.5755   90.000   90.000   90.000
      SPACE GROUP: P4_2/n    
      X-RAY WAVELENGTH:     1.541838
      Cell Volume:   1115.334
      Density (g/cm3):      3.534
      MAX. ABS. INTENSITY / VOLUME**2:      37.56262165    
      RIR:      3.461
      RIR based on corundum from Acta Crystallographica A38 (1982) 733-739
               2-THETA      INTENSITY    D-SPACING   H   K   L   Multiplicity
                10.31         82.10        8.5799    1   1   0         4
                13.78        100.00        6.4259    1   0   1         8
                14.60         12.54        6.0669    2   0   0         4
                20.13         11.83        4.4114    2   1   1         8
                20.13         14.28        4.4114    1   2   1         8
                20.70          1.19        4.2899    2   2   0         4
                23.18         20.07        3.8370    3   1   0         4
                23.49          9.61        3.7878    0   0   2         2
                24.96         16.51        3.5679    3   0   1         8
                25.71         80.43        3.4651    1   1   2         8
                27.77          4.35        3.2130    2   0   2         8
                29.03         26.16        3.0755    2   3   1         8
                29.45          7.40        3.0334    4   0   0         4
                31.51          5.03        2.8394    2   2   2         8
                32.64          4.38        2.7432    1   4   1         8
                33.24          6.02        2.6956    3   1   2         8
                36.34          2.49        2.4722    1   0   3         8
                38.97          4.78        2.3111    4   3   1         8
                39.36          1.73        2.2894    1   2   3         8
                41.83          2.93        2.1597    2   5   1         8
                42.13          1.84        2.1450    4   4   0         4
                42.19          1.79        2.1420    3   0   3         8
                43.49          2.91        2.0809    3   5   0         4
                44.88          1.55        2.0198    3   2   3         8
                44.88          1.00        2.0198    2   3   3         8
                44.99          1.17        2.0150    1   5   2         8
                47.11          3.20        1.9290    6   1   1         8
                47.39          2.59        1.9185    6   2   0         4
                47.44          1.17        1.9164    4   1   3         8
                47.44          3.55        1.9164    1   4   3         8
                48.04          5.09        1.8939    0   0   4         2
                49.59          1.40        1.8383    5   4   1         8
                51.98          1.72        1.7593    3   6   1         8
                53.54          1.06        1.7115    2   6   2         8
                56.54          1.13        1.6278    2   7   1         8
                59.01          1.96        1.5653    1   6   3         8
                61.15          2.18        1.5157    5   4   3         8
                65.25          1.64        1.4300    6   6   0         4
                65.29          1.13        1.4291    7   0   3         8
                65.82          1.10        1.4188    3   0   5         8
                67.84          2.12        1.3815    2   3   5         8
                68.40          1.79        1.3716    8   2   2         8
                68.40          2.08        1.3716    2   8   2         8
                70.25          1.16        1.3400    1   9   0         4
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       XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs
  For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.