Uranopolycrase
      Aurisicchio C, Orlandi P, Pasero M, Perchiazzi N
      European Journal of Mineralogy 5 (1993) 1161-1165
      Uranopolycrase, the uranium-dominant analogue of polycrase-(Y),
      a new mineral from Elba Island, Italy, and its crystal structure
      Locality: Elba Island, Italy
      _database_code_amcsd 0006507

      CELL PARAMETERS:   14.5100   5.5580   5.1730   90.000   90.000   90.000
      SPACE GROUP: Pbcn      
      X-RAY WAVELENGTH:     1.541838
      Cell Volume:    417.185
      Density (g/cm3):      6.599
      MAX. ABS. INTENSITY / VOLUME**2:      193.5652075    
      RIR:      9.551
      RIR based on corundum from Acta Crystallographica A38 (1982) 733-739
               2-THETA      INTENSITY    D-SPACING   H   K   L   Multiplicity
                12.20         32.11        7.2550    2   0   0         2
                24.29         30.71        3.6639    1   1   1         8
                24.40          8.76        3.6486    3   1   0         4
                24.54          7.31        3.6275    4   0   0         2
                26.55          3.02        3.3569    2   1   1         8
                29.97        100.00        2.9816    3   1   1         8
                32.21         12.67        2.7790    0   2   0         2
                34.23          1.32        2.6195    4   1   1         8
                34.56          5.66        2.5951    2   2   0         4
                34.68         11.04        2.5865    0   0   2         2
                35.25          1.27        2.5464    1   0   2         4
                36.71          4.01        2.4481    0   2   1         4
                36.89          4.17        2.4363    2   0   2         4
                37.18          7.73        2.4183    6   0   0         2
                39.11         11.33        2.3034    5   1   1         8
                40.91          7.14        2.2060    4   2   0         4
                41.34          2.43        2.1842    3   2   1         8
                42.86          1.65        2.1101    3   1   2         8
                42.95          7.47        2.1060    4   0   2         4
                46.09          1.18        1.9693    4   1   2         8
                47.06          1.47        1.9309    5   0   2         4
                48.06         10.17        1.8933    0   2   2         4
                49.77          7.06        1.8320    2   2   2         8
                50.00         10.73        1.8243    6   2   0         4
                50.17          5.67        1.8183    7   1   1         8
                50.31          1.01        1.8138    8   0   0         2
                51.75         11.27        1.7665    6   0   2         4
                52.87          6.73        1.7317    1   3   1         8
                52.92          4.64        1.7301    3   3   0         4
                53.24          6.84        1.7204    6   2   1         8
                54.68          4.03        1.6785    4   2   2         8
                56.05          6.97        1.6408    3   3   1         8
                56.21          6.28        1.6364    1   1   3         8
                57.37          1.75        1.6060    2   1   3         8
                59.27          7.62        1.5590    3   1   3         8
                61.00          1.43        1.5189    8   2   0         4
                61.87          1.06        1.4996    4   1   3         8
                62.09          2.50        1.4949    5   3   1         8
                62.28          5.68        1.4908    6   2   2         8
                62.55          1.49        1.4850    8   0   2         4
                62.63         10.86        1.4834    9   1   1         8
                63.85          1.58        1.4578    1   2   3         8
                64.84          3.08        1.4380    3   3   2         8
                65.13          2.36        1.4323    5   1   3         8
                68.79          1.62        1.3647    2   4   0         4
                70.13          1.97        1.3419    0   4   1         4
                70.57          1.95        1.3346    7   3   1         8
                72.12          1.70        1.3097    8   2   2         8
                73.43          1.88        1.2895    7   1   3         8
                74.53          1.67        1.2732    2   0   4         4
                75.62          1.27        1.2575    1   3   3         8
                78.28          2.00        1.2213    3   3   3         8
                78.67          1.15        1.2162    9   3   0         4
                79.22          2.07        1.2092   12   0   0         2
                79.39          1.89        1.2070    2   4   2         8
                81.26          2.02        1.1839    9   3   1         8
                82.14          2.44        1.1734    6   4   1         8
                83.32          1.21        1.1598    4   4   2         8
                83.52          1.69        1.1575    2   2   4         8
                83.52          1.97        1.1575    5   3   3         8
                84.00          2.50        1.1521    9   1   3         8
                84.04          1.56        1.1517   10   2   2         8
                87.42          1.58        1.1157    4   2   4         8
                88.10          1.24        1.1088   12   2   0         4
                88.93          1.06        1.1006    9   3   2         8
                89.46          1.30        1.0954   12   0   2         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.