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
In the Seibert microscope eye-piece No. 0 is used for most purposes.
Other eye-pieces, Nos. 1 and 2, with cross-wires, are used for
different degrees of magnification, and one eye-piece, No. 3, without
cross-wires, is provided to be used in connection with an eye-piece
micrometer.
Footnote 27:
With the Seibert microscope, Fig. 2, the No. 0 eye-piece and the No.
II objective will prove most satisfactory for the following tests.
With the Fuess microscope use No. 4 objective. With an English
microscope use an ordinary eye-piece and a 1″ or ¾″ objective.
Footnote 28:
Twins may be recognized just as in macroscopic specimens, and zonal
structure noticed if the zones differ in color. When a colorless
mineral is surrounded by other colorless minerals, of about the same
index of refraction, its outline is often best brought out by
observation between crossed nicols.
Footnote 29:
The term “Anhedron,” meaning without planes, has been suggested by L.
V. Pirsson to describe in rocks the crystal fragments which have no
plane faces, as, for example, the augites of augitic rocks. _Science_,
Jan. 10, 1896, p. 49.
Footnote 30:
Partial resorption and recrystallization may produce a border of
secondary minerals, surrounding the original crystal.
Footnote 31:
The surfaces of all minerals in sections are more or less rough, but
this roughness is only made visible when there is a marked difference
between the indices of refraction of the minerals, and the index of
refraction of the balsam in which the minerals are embedded. The index
of refraction of balsam is about 1.54, so it is only when the mineral
has a higher or lower index of refraction that its surface appears
rough. When internal structure is to be studied, the crystal should be
surrounded by a fluid of nearly the same index of refraction as that
of the crystal, and when the exterior of the crystal is to be studied,
then a fluid should be used with a very different index of refraction.
Footnote 32:
The Seibert microscope has a very convenient and quick lowering
adjustment, by means of the lever _d_, for making this test. For
convenience the lower nicol and condensing lens are generally left in
place below the stage of the microscope, as polarized light serves as
well for these investigations as ordinary light. An additional
advantage in this arrangement is that the condensing lens is always
ready for the “relief” test and the lower nicol for the pleochroism
test; but it must be remembered that the polarizer or lower nicol cuts
out one half of the light, which comes to it from the reflector, and
this loss is important when high power objectives are to be used. When
very low power objectives are used, the condensing lens must be
removed.
Footnote 33:
_Mem. de l’Acad._, Paris, 1767–68.
Footnote 34:
_Min. Mag._, Vol. I., p. 193; Vol. II., p. 1.
Footnote 35:
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