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Minerals in rock sections

Chapter 6: CONVENTIONS AND ABBREVIATIONS.
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About This Book

The book provides a practical handbook for identifying rock-forming minerals under the microscope by presenting essential optical theory, descriptions of petrographic microscope components, and step-by-step investigation techniques. It explains light behavior in crystals, methods for measuring refractive indices and birefringence (including Becke and van der Kolk procedures), interpretation of pleochroism, interference colors, extinction angles and interference figures, and criteria for distinguishing crystal systems. Individual minerals are described by their microscopic characters and typical appearances in thin section. Chapters also cover preparing and mounting thin sections, useful tables and diagrams, and simple chemical and mechanical tests.

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.

2E = the apparent axial angle measured in air, 2V being the true angle.

Bx = The acute bisectrix.

Bx = The obtuse bisectrix.

Ax. pl. = The axial plane, i. e., the plane containing the two “optic axes.”

Elongation relates to the appreciable extension often shown by the crystal section. A crystal of long prismatic habit, cut about parallel to the ć axis, would show marked elongation; while a tabular crystal (like mica) would show elongation if cut at right angles to the tabular faces. At times, of course, no elongation is appreciable, as in the case of granular or broken crystals or where the cross-section is essentially square or octagonal. Very often the relation of the cleavage is given to the elongation and also to the directions a′ and c′, which makes it possible to test for a′ and c′ even when no marked elongation can be observed.