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Minerals in rock sections

Chapter 4: PREFACE TO REVISED EDITION, 1905.
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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.

PREFACE TO REVISED EDITION, 1905.

In preparing the revised edition, Chapters I. and IV. have been rewritten and enlarged and the part relating to the determination of the plagioclases has been greatly amplified. Many additions have also been made to Chapter III. and the Becke method, for the determination of the relative indices of refraction of minerals, has been given in detail.

Some new and useful tables have been introduced; as tables of refractive indices (mean) and double refraction (maximum). A diagram has also been added, showing the relation existing between strength of double refraction, interference colors and thickness of section.

Professor E. Weinschenk’s admirable text-book, “Die Gesteinsbildenden Mineralien”, Freiburg, 1901, has been specially referred to, and the tables of refractive indices and double refraction have been compiled from Weinschenk’s new Tables.

Many new cuts have been added, among them being semi-ideal drawings, showing typical outlines of crystal sections, cleavage, optical orientation, etc. In describing the “Usual Appearance in Sections” of a mineral, it is of course only possible to mention the usual crystal form in which the mineral occurs in a rock. The crystal may be cut in any way by the plane of the section; but a general knowledge of the crystal forms will furnish an idea as to the outline, etc., that the mineral may show in the section.

Lea McI. Luquer.
Department of Mineralogy,
Columbia University, New York, July, 1905.