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
For most cases in observations with white light the “optics axes” may
be regarded as approximately fixed in position.
Footnote 15:
Often spoken of as: a, the axis of maximum; b, the axis of
intermediate, and c, the axis of minimum elasticity.
In the more recent American text-books on Optical Mineralogy by
Iddings, Winchell and Phillips a is denoted by _X_, b by _Y_ and c by
_Z_.
Footnote 16:
For a short historical sketch of the use of the microscope in
connection with Petrology, see G. H. William’s pamphlet, _Modern
Petrography (Monographs of Education)_, Boston, 1886. For detail
description and adjustments, see _Methods of Petrographic-Microscopic
Research_, F. E. Wright, 1911, pp. 11, 61.
Footnote 17:
For description of the ordinary microscope, eye-pieces, objectives,
magnification, etc., see _Manipulation of the Microscope_, by Ed.
Bausch.
Footnote 18:
Text Book of Mineralogy, by E. S. Dana, 1898 Ed., p. 176.
Footnote 19:
It is convenient to assume that the vibrations of the polarized light
are taking place in this plane, called the “plane of vibration,” but
all the phenomena caused by polarized light could be also explained on
the assumption that the vibrations were taking place at right angles
to this plane.
Footnote 20:
This condensing lens must be removed when very low power objectives
are used.
Footnote 21:
Some microscopes are provided with adjusting screws bearing on the
frame holding the objective, which can then be accurately centered to
the axis of rotation of the stage.
Footnote 22:
In the Seibert microscope use objective No. 00 for the first general
study of a rock section, No. II for general use and No. V for
observations with convergent light. In the Fuess microscope use
objective No. 4 for general use and No. 7 for convergent light tests.
In the case of an English microscope a 1″ to ¾″ objective is used for
general purposes and a ¼″ to ⅕″ for observations with convergent
light.
Footnote 23:
See pp. 33 and 34.
Footnote 24:
In some microscopes the analyzer is in the form of a “cap” nicol,
arranged to be fitted over the top of the eye-piece, and not
introduced in the microscope tube as shown here. This form is not so
convenient, as the “cap” nicol must be set by hand every time it is
desired to make observations with crossed nicols. But at the same time
it avoids any possible refocusing which may be necessary when the
other type of analyzer is introduced in the tube.
Footnote 25:
When accurate adjustments are possible of the vibration planes of the
nicols and the cross-wires parallel to these vibration planes,
reference should be made to _Methods of Petrographic-Microscopic
Research_, p. 61, 1911, Fred. E. Wright.
Footnote 26:
Public-domain text, read in full here on John Shaqi.
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