CHAPTER VI.. Chemical and Mechanical Tests.

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.

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; 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{a·}_ = The acute bisectrix.

Bx{c·}_ = 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.

MINERALS IN ROCK SECTIONS.