Page 61 - 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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