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
The (+) and (−) character is easily determined by remembering that the
line, joining the dark spots, makes the + and − sign respectively with
the direction c of the mica plate. The direction c of the mica plate
(represented in the figures by an arrow) is of course not seen, but its
position must be borne in mind when making this test. This test can be
made with either monochromatic or white light.
If the mica plate does not give satisfactory results, which will be the
case when the double refraction of the crystal to be tested is very weak
or when the section is very thin, use a selenite plate, cut the proper
thickness to give the red color of the first order.
This plate must be introduced with its vibration direction a (previously
determined) making an angle of 45° with the planes of vibration of the
nicols. Instead of the dark spots being seen there will appear two blue
and two red quadrants. The diagonally opposite quadrants being of the
same color.
In determining the (+) and (−) character consider the blue quadrants as
the equivalent of the dark spots in the preceding case. This test must
be made with white light.[72]
Biaxial Interference Figures.
[Illustration:
FIG. 28.
]
[Illustration:
FIG. 29.
]
(_a_) Sections perpendicular to an optic axis exhibit the interference
figures shown in Figs. 28 and 29, the curves being nearly circular and a
straight black bar bisecting these curves, whenever the trace of the
plane of the optic axes coincides with the vibration direction of either
nicol. As the stage, carrying the section, is rotated the bar changes
into one arm of a hyperbola and back again into a bar. This arm or bar
will rotate in the opposite direction to the motion of the stage.
As previously stated sections of biaxial crystals, perpendicular to an
optic axis, do not remain dark during rotation of the stage between
crossed nicols in parallel light. On the contrary these sections remain
uniformly illuminated.[73]
(_b_) Sections perpendicular to the acute bisectrix (see p. 5), exhibit
interference figures like those shown in Figs. 30 and 31.
[Illustration:
FIG. 30.
]
[Illustration:
FIG. 31.
]
Fig. 30 shows the appearance of the interference figure when the plane
of the optic axes is parallel to the plane of vibration of either nicol,
and Fig. 31 shows the appearance when this plane is inclined 45° to the
planes of vibration of the nicols.
As the stage, carrying the section, is rotated the dark cross seems to
dissolve into two branches of a hyperbola, which again unite to form a
cross.
In sections perpendicular to a bisectrix, with a large axial angle, the
figure will appear, during a rotation of 90° (in the direction of the
hands of a watch), as in Fig. 32, top row. When the section is somewhat
oblique to an “optic axis,” the figure appears as in middle row; and
when still more oblique, as in bottom row.
Public-domain text, read in full here on John Shaqi.
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