Minerals in rock sections : $b The practical methods of identifying minerals in rock sections with the microscope, especially arranged for students in technical and scientific schoolsLuquer, Lea McIlvaine
Science
Minerals in rock sections : $b The practical methods of identifying minerals in rock sections with the microscope, especially arranged for students in technical and scientific schools
Luquer, Lea McIlvaine
Petrology -- Laboratory manuals
FIG. 22.—Olivine decomposed to serpentine. The pseudomorphism has been
almost complete, only small portions of the original olivine
remaining. The outline of the parent crystal can be quite distinctly
seen. Crossed nicols.
]
(_e_) _Pseudomorphic_ structure, which may be partial or complete and is
noticed by the changed portions producing different optical effects from
those of the original mineral. Sometimes, although the pseudomorphism
has been almost complete, the form of the original mineral or crystal
may still be seen, Fig. 22.
Characters Observed by Convergent Polarized Light.
_Convergent light_ is obtained by passing the rays of polarized light
through a strong condensing lens, which generally fits like a cap over
the top of the polarizer. By means of a suitable adjustment the
condensing lens can be brought very close to the lower surface of the
section on the stage. The lens thus sends a cone of light through the
section, and used in connection with _crossed nicols_ a series of
optical phenomena, called _interference figures_,[68] are produced.
Each direction in which rays are sent is traversed by a minute bundle of
parallel rays and these rays extinguish and produce interference colors
as already described for parallel light. Hence each direction yields a
spot or picture in the field of view and from all these spots combined
there results an “interference figure” or picture, depending upon the
structure of the section for all the directions traversed by the rays.
A very high power objective[69] must be used, and when the eye-piece is
removed, a small image of the interference figure will be seen. In some
microscopes an arrangement is made for getting a magnified image of the
interference figure, by retaining the eye-piece and using an additional
Bertrand lens.
In order to get good results care must be taken to have strong
illumination and the condensing lens close up under the section. The
tests are best made with monochromatic light, but with white light the
effects are substantially the same, the only difference being that the
rings and curves are variously colored instead of being simply light and
dark.
_Isotropic_ substances show no _interference figures_.
Uniaxial Interference Figures.
(_a_) Sections perpendicular to the optic or vertical axis _ć_ show a
dark cross, with or without colored rings, Figs. 23 and 24. The figure
is symmetrical to the center, as the optical behavior of uniaxial
crystals is symmetrical to the optic axis.
[Illustration:
FIG. 23.
]
[Illustration:
FIG. 24.
]
The arms of the cross are parallel to the planes of vibration of the
nicols, and the figure does not move when the stage carrying the section
is rotated.[70]
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