Computational Mineral Physics : A Practical Guide for Earth Scientists
Book Details
Format
Hardback or Cased Book
ISBN-10
1108416772
ISBN-13
9781108416771
Publisher
Cambridge University Press
Imprint
Cambridge University Press
Country of Manufacture
GB
Country of Publication
GB
Publication Date
Jun 11th, 2026
Print length
332 Pages
Weight
837 grams
Product Classification:
Condensed matter physics (liquid state & solid state physics)Condensed matter physics (liquid state and solid state physics)GeophysicsChemistryPetrologyPetrology, petrography and mineralogyGeochemistryNanotechnologyEnvironmental science, engineering & technologyEnvironmental science, engineering and technology
Ksh 12,800.00
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Written in a user- and property-oriented way, this book is for geoscientists seeking an introductory guide to performing first-principles calculations, as well as researchers working in a lab, those seeking to identify minerals remotely or in the field, and those seeking specific numerical values of particular physical properties.
Computational mineralogy is fast becoming the most effective and quantitatively accurate method for successfully determining structures, properties and processes at the extreme pressure and temperature conditions that exist within the Earth's deep interior. It is now possible to simulate complex mineral phases using a variety of theoretical computational techniques that probe the microscopic nature of matter at both the atomic and sub-atomic levels. This introductory guide is for geoscientists as well as researchers performing measurements and experiments in a lab, those seeking to identify minerals remotely or in the field, and those seeking specific numerical values of particular physical properties. Written in a user- and property-oriented way, and illustrated with calculation examples for different mineral properties, it explains how property values are produced, how to tell if they are meaningful or not, and how they can be used alongside experimental results to unlock the secrets of the Earth.
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