Page 60 - A Practical Introduction to Optical Mineralogy
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AMPHIBOLE  GROUP

                              (a)
                                    71 I                                                                                         Common hornblende
                                   +    !
                                     II--                                                                                        2V" variable, usually large, but
                                           ;---r-- 2Va1
                                                  ..............                                                                 2 V"  for  hastingsite  is very small :
                                     I                                                                                010
                                                      ............                                                               pargasite  has -y  as acute
                                                        ~                                                                        bisectri x and is +ve
                                 <U   )(  I
                                 Oil                        "'-..
                                 c                             ~
                                 ~
                                 :::.   :11  I I--                ]"-.,
                                 N
                                    II  I
                                   1.7  4
                                                                  ~                                                   ------b =  [3
                                   1.7  2
                                                               ~
                                                            ~
                                                          ./.
                                 .Q  1.7(  I            v      v
                                 u                 11/  ~ v
                                 ..t  1.6  X            v
                                                  ....;:;-~
                                 ~           /   ~ v
                                 0  1.66   [/::  v v
                                 X                 n"
                                 u
                                    ,V v
                                   1.6
                                 v  c  4v   ]:7
                                   1.6  -v
                                                                                                    n.  =  L615- L70S} T_he large variati?n in  RI is due to comp.osi.tional
                                   1.61 I                                                           n  =  L6 S-L7Z 9   differences,  particularly  the  Mg : Fe  ratiO  m  the
                                                                                                           1
                                   1.5X                                                             n: =  L632- L o  hornblende.  Ferric iron and  aluminium in  the Z
                                                                                                               73
                                     \lXI   90   XO   70   60   50   40   30   20   I 0   0           =  o.o _0.02B   sites  will  also affect  both Rls and 2V
                                                                                                    0      14
                                         100 x Mg:(Mg +  Fe2+  +  FeH  +  Mn)
                                              'Common' hornblende                                   2V.  =  15°-90° - ve (Mg hornblendes are  +ve with 2V, almost 90°)
                                                                                                    OAP is  parallel to (010)
                                                                                                    D =  3.02-3.50   H  =  5-6
                                                                                              coLouR  Variable,  light  brown or green  but much  darker colours for  iron-rich
                                                                   Key
                            (b)                                                                     varieties.
                                          Na atoms               P a parga  site          •1•J EOCHROISM  Variable with a  pale brown or green, {3  andy brown green.  Iron-rich
                                                                 Ed cdcni te
                            Pa        Ed          Ed       Pa    Ts tsche  nnakitc                  varieties have a yellow brown or green, {3  deep green or blue green, and
                                                1         1'-.   !-Ia  hasti  ngsitc                y  very dark green.
                                                 "'        I                                   HABIT  Prismatic crystals common,  usually  elongate.
                                                             ""
                                                   ""'     I                                        { 100}  and { 001}  may also be present.
                              hornblende             ""'-hornblende""'-                     •n  EAVAGE  Usual  amphibole  cleavages  (see  introduction).  Partings  parallel  to
                           Ts          !-Ia            ""  "'.li-l a   ""   Ts                 RELIEF  Moderate to high.
                                                 ()                """                      AI 1 ERATION  See introductory section.
                                                                                          JII KJ I·KINGENCE  Moderate: maximum interference colours are low second order blues,
                            ~-- AI atoms (replacing Si)   AI atoms (replacing Mg)  --..
                                                                                                    but these  are frequently  masked by the body colour, especially if the
                                                                                                    hornblende is  an  iron- or sodium-rich variety.
                                                                                          IN II RII,RENCE
                                                                                               HGURE  Similar to tremolite-actinolite with extinction angle y'cl  up to 30° (see
                         Figure 2.6  (a) Variation of 2V angle and indices of refraction in  the 'common'   I  IINC'TION  .   .
                         hornblende series  (after  Deer,  Howie &  Zussman  1962)  (b) field  of common   ANGLE  IntroduCtiOn).
                         hornblende compositions.                                            I WINNING  1
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