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Sedimentary Rocks in the Field - Dorrik A.V. Stow

Sedimentary Rocks in the Field

A Color Guide
Buch | Softcover
320 Seiten
2005
Academic Press Inc (Verlag)
978-0-12-369451-5 (ISBN)
CHF 57,60 inkl. MwSt
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The must have field companion featuring more than 450 colour photographs and illustrations. Contains extensive cross referencing for ease of use in the field and examples from more than 30 countries.
Sediments and sedimentary rocks cover 70% of the Earth's surface, and make up a significant portion of the geological record. Understanding the processes (physical, chemical and biological) that lead to formation of sedimentary material is key in disciplines ranging from geology to environmental science to archaeology. But before interpretation must come observation and identification: Stow's Field Guide is a must-have for this distinctly visual process

Professor Stow has culled his extensive research experience into a succinct guide designed for students and professionals in geophysics, geochemistry, paleontology, soil sciences, environmental sciences and more. Sections on field techniques and reader-friendly descriptions also make this guide accessible to amateur geologists.

Contents:

Preface
Acknowledgemnets
1 Overview
2 Field Techniques
3 Principal Characteristics of Sedimentary Rocks
4 Conglomerates
5 Sandstones
6 Mudrocks
7 Carbonate Rocks
8 Cherts and Siliceous Sediments
9 Phosphorites
10 Coal and Oil
11 Evaporites
12 Ironstones
13 Soils, Paleosols, and Duricrusts
14 Volvaniclastic Sediments
15 Interpretations and Depositional Environments
References and Key Texts
Metric-Imperial Conversions
Index
Appendices
– Stratigraphic Timescale
– Mapping Symbols
– Grain-Size Comparator Chart
– Sediment Description Checklist
– Wulff Stereonet
– Lambert Equal-Area Projection

Erscheint lt. Verlag 12.6.2005
Verlagsort San Diego
Sprache englisch
Maße 146 x 210 mm
Gewicht 590 g
Themenwelt Naturwissenschaften Geowissenschaften Geologie
ISBN-10 0-12-369451-5 / 0123694515
ISBN-13 978-0-12-369451-5 / 9780123694515
Zustand Neuware
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