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
CHAPTER V.
METHODS OF PREPARING SECTIONS.
Cutting and Grinding Machines.—Saws.—Cutting.—Grinding. Plates or
Laps.—Cementing.—Grinding.—Mounting.—Cleaning and
Finishing.—Convenient Apparatus for work. 117
CHAPTER VI.
CHEMICAL AND MECHANICAL TESTS.
Chemical Tests on Crystal in Section: _Carbonates_, _Gelatinizing
Silica_.—Etched Figures.—Heating Section to Redness.—Methods of
Isolating Crystals or Fragments for Testing: _Specific Gravity
Separation_, _Electro-magnetic Separation_, _Chemical
Separation_.—Micro-Chemical Reactions: _Borichy’s Method_,
_Behren’s Method_, _Special Tests_. 129
APPENDIX.
Brief Scheme of Classification into Systems by Optical
Determinations.—Tables of Double Refraction (maximum) and
Indices of Refraction (mean).—Diagram, showing relation between
strength of double refraction, interference colors and
thickness of section.—Order of Consolidation of the Constituent
Minerals in Plutonic Rocks.—Optical Scheme with Special
Introduction. 141
INDEX. 149
CONVENTIONS AND ABBREVIATIONS.
a = The assumed direction of the ether vibrations of the fastest ray.
b = The assumed direction of the ether vibrations of the ray with
intermediate velocity.
c = The assumed direction of the ether vibrations of the slowest ray.
In some American Text-Books (by Iddings, Winchell & Phillips) a = X, b =
Y and c = Z.
a′ = The assumed direction of the ether vibrations of the faster ray in
the given section.[1]
c′ = The assumed direction of the ether vibrations of the slower ray in
the given section.
(+) = Optical character positive.
(−) = Optical character negative.
|| = Parallel to.
(γ − α) = The difference between the indices of refraction of the
slowest and fastest rays, respectively, transmitted by the crystal, and
indicates in decimals the relative strength of the double refraction.
_n′_ = The mean index of refraction;[2] hence
= (α + β + γ)/3 or (ε + 2ω)/3.
α = Index of refraction of the fastest ray.
γ = Index of refraction of the slowest ray.
_a_, _b_ and _ć_ relate to the crystallographic axes commonly
represented by these letters.
2_E_ = the apparent axial angle measured in air, 2_V_ being the true
angle.
_Bx_{a·}_ = The acute bisectrix.
_Bx_{c·}_ = The obtuse bisectrix.
_Ax. pl._ = The axial plane, _i. e._, the plane containing the two
“optic axes.”
Public-domain text, read in full here on John Shaqi.
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