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  • © 1979

Petrogenesis of Metamorphic Rocks

Part of the book series: Springer Study Edition (SSE)

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Table of contents (18 chapters)

  1. Front Matter

    Pages i-x
  2. Definition and Types of Metamorphism

    • Helmut G. F. Winkler
    Pages 1-8
  3. From Diagenesis to Metamorphism

    • Helmut G. F. Winkler
    Pages 9-14
  4. Factors of Metamorphism

    • Helmut G. F. Winkler
    Pages 15-27
  5. The Four Divisions of Metamorphic Grade

    • Helmut G. F. Winkler
    Pages 64-96
  6. General Characteristics of Metamorphic Terrains

    • Helmut G. F. Winkler
    Pages 97-110
  7. Metamorphic Reactions in Carbonate Rocks

    • Helmut G. F. Winkler
    Pages 111-139
  8. Metamorphism of Marls

    • Helmut G. F. Winkler
    Pages 140-153
  9. Metamorphism of Mafic Rocks

    • Helmut G. F. Winkler
    Pages 168-203
  10. Very-Low-Grade Metamorphism of Graywackes

    • Helmut G. F. Winkler
    Pages 204-205
  11. Metamorphism of Pelites

    • Helmut G. F. Winkler
    Pages 206-238
  12. Regional Hypersthene Zone (Granolite High-Grade)

    • Helmut G. F. Winkler
    Pages 256-275
  13. Eclogites

    • Helmut G. F. Winkler
    Pages 276-282
  14. Back Matter

    Pages 340-348

About this book

The first edition of this book was published in 1965 and its French translation in 1966. The revised second edition followed in 1967 and its Russian translation became available in 1969. Since then, many new petrographie observations and experimental data elucidating reactions in metamorphie rocks have made a new approach in the study of metamor­ phic transformation desirable and possible. It is feIt that this new approach, attempted in this book, leads to a better understanding of rock metamorphism. The concept of metamorphie facies and subfacies considers asso­ cations of mineral assemblages from diverse bulk compositions as char­ acteristie of a certain pressure-temperature range. As new petrographie observations accumulated, it became increasingly difficult to accommo­ date this information within a manageable framework of metamorphic facies and subfacies. Instead, it turned out that mineral assemblages due to reactions in common rocks of a particular composition provide suita­ ble indieators of metamorphie conditions. Metamorphic zones, defined on the basis of mineral reactions, very effectively display the evolution of metamorphic rocks. Thus, the importance of reactions in metamor­ phic rocks is emphasized. Experimental calibration of mineral reactions makes it possible to distinguish reactions which are of petrogenetic sig­ nificance from those which are not. This distinction provides guidance in petrographie investigations undertaken with the object of deducing the physieal conditions of metamorphism. Within a metamorphie terrain, points indicating the same reaction constitute a line or a band, here designated by the term isoreaction-grad.

Authors and Affiliations

  • Institute of Mineralogy and Petrology, University of Göttingen, Federal Republic of Germany

    Helmut G. F. Winkler

Bibliographic Information

  • Book Title: Petrogenesis of Metamorphic Rocks

  • Authors: Helmut G. F. Winkler

  • Series Title: Springer Study Edition

  • DOI: https://doi.org/10.1007/978-1-4757-4215-2

  • Publisher: Springer New York, NY

  • eBook Packages: Springer Book Archive

  • Copyright Information: Springer Science+Business Media New York 1979

  • eBook ISBN: 978-1-4757-4215-2Published: 29 June 2013

  • Series ISSN: 0172-6234

  • Edition Number: 5

  • Number of Pages: X, 348

  • Number of Illustrations: 63 b/w illustrations

  • Topics: Mineralogy, Geochemistry

Buy it now

Buying options

eBook USD 74.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever

Tax calculation will be finalised at checkout

Other ways to access