Description

Book Synopsis

Here is a comprehensive and up to-do-date presentation of the origins, and properties of clay minerals at the Earth´s surface. The text reviews the relatively simple laws that govern the chemical or isotopic composition and the crystalline structure of clays, and then discusses their genesis and alteration. Concluding chapters show that clay minerals can form in variety of different environments: meteorites, lavas, subduction zones, among others.



Table of Contents
Crystal Structure — Species — Crystallisation.- Crystal Chemistry of Clay Minerals.- Energy Balances: Thermodynamics — Kinetics.- Isotopic Composition of Clay Minerals.- Surface Properties — Behaviour Rules — Microtextures.- Clays in Soils and Weathered Rocks.- Clays in Sedimentary Environments.- Diagenesis and Very Low-Grade Metamorphism.- Hydrothermal Process — Thermal Metamorphism.- Clays Under Extreme Conditions.

Clays

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    A Hardback by Alain Meunier

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      Book details

      Publisher Springer-Verlag Berlin and Heidelberg GmbH & Co. KG
      Published 13 January 2005
      ISBN-13 9783540216674
      978-3540216674
      ISBN-10 3540216677
      Also in:
      Geochemistry Geology, geomorphology and the lithosphere Petrology, petrography and mineralogy

      Description

      Book Synopsis

      Here is a comprehensive and up to-do-date presentation of the origins, and properties of clay minerals at the Earth´s surface. The text reviews the relatively simple laws that govern the chemical or isotopic composition and the crystalline structure of clays, and then discusses their genesis and alteration. Concluding chapters show that clay minerals can form in variety of different environments: meteorites, lavas, subduction zones, among others.



      Table of Contents
      Crystal Structure — Species — Crystallisation.- Crystal Chemistry of Clay Minerals.- Energy Balances: Thermodynamics — Kinetics.- Isotopic Composition of Clay Minerals.- Surface Properties — Behaviour Rules — Microtextures.- Clays in Soils and Weathered Rocks.- Clays in Sedimentary Environments.- Diagenesis and Very Low-Grade Metamorphism.- Hydrothermal Process — Thermal Metamorphism.- Clays Under Extreme Conditions.

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