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
(_b_) Sections oblique to the optic axis show a portion of a dark cross,
with or without colored rings, Fig. 25. The centre of the cross is not
in the axis of rotation, and as the stage bearing the section is
revolved, the centre of the cross describes a circle, the arms always
maintaining parallel positions.
If the section is still more oblique to the optic axis the centre of the
interference cross may be outside the field of view, and only portions
of the dark arms will be seen.
Sections parallel to the optic axis show a vague dark cross, which, on
rotating the stage, dissolves into hyperbolic curves (suggesting biaxial
figure), which very rapidly disappear in the direction of the optic
axis. When the interference figure shows colors, these colors are lower
in order in the quadrants containing the optic axis. Knowing thus the
position of the optic axis the optical character can be obtained by the
method for parallel light, p. 43.
[Illustration:
FIG. 25.
]
Sections which are thick and have strong double refraction will show the
cross and rings clearly and sharply defined, there being quite a number
of rings crowded close together. Sections which are very thin and have
weak double refraction show only a broad dark cross and no rings. The
interference figures will vary between these extremes, depending on the
thickness of the section and the strength of the double refraction.
To obtain the most characteristic figures, observations must be made on
sections about perpendicular to the optic axis, that is sections which
remain dark or nearly dark during complete rotation between crossed
nicols in parallel light.
▄Optical Character, Positive or Negative.▄ After having obtained an
uniaxial interference figure, test it by means of a ¼ undulation mica
plate. This plate must be introduced between the objective[71] and the
analyzer in such a way that its vibration direction c, marked on the
plate, makes an angle of 45° with the planes of vibration of the nicols.
When this is done the interference figure changes, or may more or less
disappear, two dark spots or blotches being brought prominently into
view. If rings are still seen it will be noticed that they have expanded
in the quadrants occupied by the dark spots, and have contracted in the
remaining quadrants. This movement of the rings may make it possible to
determine the optical character of a section, which is so oblique to the
optic axis that the dark spots are not seen after the introduction of
the mica plate.
[Illustration:
FIG. 26.
]
[Illustration:
FIG. 27.
]
If the optical character is _positive_ the line joining these dark spots
is perpendicular to the direction c of the mica plate, see Fig. 26.
If _negative_ the line joining the dark spots coincides with the
direction c of the mica plate, see Fig. 27.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account