Condition: Good. Volume 4A. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. In good all round condition. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,1850grams, ISBN:9781862390812.
Language: English
Published by Geological Society of London, 2001
ISBN 10: 1862390819 ISBN 13: 9781862390812
Seller: Geology, Livermore, CA, U.S.A.
Hardcover. Condition: As New. 2nd Edition. Rewritten and expanded upon from first edition with advances in knowledge and technology includes summarization of important research results. Chapters are headed by a brief tabulation of mineral data and sketches showing optical orientation, and contains full references to the literature. Diagrams of crystal structures are presented and followed by a discussion of the structure features, making use of data from spectroscopic as well as diffraction experiments. The chemical sections include many analyses from which structural formulae have been calculated, illustrating the range of chemical and paragenetic variation exhibited by each mineral: also the results of P-T experiments and thermochemical and computer modelling techniques.
Language: English
Published by Geological Society of London, 2001
ISBN 10: 1862390819 ISBN 13: 9781862390812
Seller: WeSavings LLC, MONTGOMERY, TX, U.S.A.
Hardcover. Condition: Very Good. No Jacket. Very good condition, appears unread. X-Library book. Typical library markings. Ships promptly from Texas. 100% Money-Back Guarantee!!!
Language: English
Published by Geological Society Pub House, 2001
ISBN 10: 1862390819 ISBN 13: 9781862390812
Seller: Revaluation Books, Exeter, United Kingdom
Hardcover. Condition: Brand New. 2nd edition. 992 pages. 9.75x6.75x2.00 inches. In Stock.
Language: English
Published by Geological Society of London, 2001
ISBN 10: 1862390819 ISBN 13: 9781862390812
Seller: Mispah books, Redhill, SURRE, United Kingdom
Hardcover. Condition: New. NEW. SHIPS FROM MULTIPLE LOCATIONS. book.