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Thermodynamics in Geology

Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976

  • Donald G. Fraser

Part of the NATO Advanced Study Institutes Series book series (ASIC, volume 30)

Table of contents

  1. Front Matter
    Pages I-XIII
  2. E. J. W. Whittaker
    Pages 99-113
  3. Niranjan D. Chatterjee
    Pages 137-159
  4. David R. Wones, Franklin C. W. Dodge
    Pages 229-247
  5. Donald G. Fraser
    Pages 301-325
  6. R. K. O’Nions, R. Powell
    Pages 349-363
  7. Wallace S. Broecker, Taro Takahashi
    Pages 365-379
  8. George W. Fisher
    Pages 381-403
  9. Back Matter
    Pages 405-410

About these proceedings

Introduction

It has long been realized that the mineral assemblages of igneous and metamorphic rocks may reflect the approach of a rock to chemical eCluilibrium during its formation. However progress in the application of chemical thermodynamics to geological systems has been hindered since the time of Bowen and the other early physical-chemical petrologists by the recurring Cluandary of the experimental geologist. His systems are complex and are experimentally intractable, but if they were not so refractory they would not be there to study at all. It is only recently that accurate measurements of the thermodynamic properties of pure, or at least well-defined minerals, melts and volatile fluid phases, combined with experimental and theoretical studies of their mixing properties, have made it possible to calculate the eCluilibrium conditions for particular rock systems. Much work is now in progress to extend the ranges of com­ position and conditions for which sufficient data exist to enable such calculations to be made. Moreover the routine availability of the electron microprobe will ensure that the demand for such information will continue to increase. The thermodynamic techniClues reCluired to apply these data to geological problems are intrinsically simple and merely involve the combination of appropriate standard state data together with corrections for the effects of solution in natural minerals, melts or volatile fluids.

Keywords

Pet Vine behavior calorimetry chemistry element energy equation of state geology microscopy mineral phase diagram stability structure thermodynamics

Editors and affiliations

  • Donald G. Fraser
    • 1
  1. 1.Dept. of Geology and MineralogyUniversity of OxfordEngland

Bibliographic information

  • DOI https://doi.org/10.1007/978-94-010-1252-2
  • Copyright Information Springer Science+Business Media B.V. 1977
  • Publisher Name Springer, Dordrecht
  • eBook Packages Springer Book Archive
  • Print ISBN 978-90-277-0834-2
  • Online ISBN 978-94-010-1252-2
  • Series Print ISSN 1389-2185
  • Buy this book on publisher's site