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Rock-forming Minerals in Thin Section

Autor Hans Pichler, Cornelia Schmitt-Riegraf
en Limba Engleză Hardback – 31 mai 1997
Identificationof rock-forming minerals in thin section is a key skill needed by all earth science students and practising geologists. This translation of the completely revised and updated German second edition (by Leonore Hoke, Institute of Geological and Nuclear Sciences, New Zealand) provides a comprehensive guide to identifying 140 of the most important rock-forming mineral species.
The book is divided into three main parts. Part A is a practical guide to the fundamentals of crystal optics, polarization microscopy and the practical use of microscopes. Part B gives a detailed description of the characteristic optical features, special features, and the paragenesis of the most common rock-forming minerals. This well-illustrated part is divided into opaque minerals, isotropic, uniaxial and optical biaxial mineral groups. Part C contains identification tables for the minerals and diagrams showing the international classification of magmatic rocks, as well as a colour plate section showing crystal forms of minerals.
The book will provide an invaluable guide to all undergraduate earth scientists, as well as to professional geologists requiring an overview of mineral identification in thin section.
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Specificații

ISBN-13: 9780412644603
ISBN-10: 0412644606
Pagini: 244
Ilustrații: X, 220 p.
Dimensiuni: 183 x 260 x 20 mm
Greutate: 0.66 kg
Ediția:Second Edition 1997
Editura: Springer
Locul publicării:Dordrecht, Netherlands

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Cuprins

A Optical Crystallography.- 1 The polarizing microscope.- 2 Orthoscopic observations.- 3 Observations under conoscopic light.- B Optical Mineralogy.- 1 Opaque minerals and substances.- 2 Optically isotropic (also pseudocubic) minerals and amorphous substances.- 3 Optically uniaxial minerals.- 4 Biaxial crystals.- C Appendices.- 1 Tables for the microscopic identification of rock-forming minerals.- 2 Diagrams for the classification of magmatic rocks.- 3 Diagrams of mineral and rock structures.