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Petrogenesis of Metamorphic Rocks

  • Helmut G. F. Winkler

Part of the Springer Study Edition book series (SSE)

Table of contents

  1. Front Matter
    Pages i-x
  2. Helmut G. F. Winkler
    Pages 1-8
  3. Helmut G. F. Winkler
    Pages 9-14
  4. Helmut G. F. Winkler
    Pages 15-27
  5. Helmut G. F. Winkler
    Pages 64-96
  6. Helmut G. F. Winkler
    Pages 97-110
  7. Helmut G. F. Winkler
    Pages 111-139
  8. Helmut G. F. Winkler
    Pages 140-153
  9. Helmut G. F. Winkler
    Pages 168-203
  10. Helmut G. F. Winkler
    Pages 204-205
  11. Helmut G. F. Winkler
    Pages 206-238
  12. Helmut G. F. Winkler
    Pages 256-275
  13. Helmut G. F. Winkler
    Pages 276-282
  14. Back Matter
    Pages 340-348

About this book

Introduction

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.

Keywords

Metamorphose Paragenesis classification diagenesis formation granite metamorphism mineral petrogenesis petrography

Authors and affiliations

  • Helmut G. F. Winkler
    • 1
  1. 1.Institute of Mineralogy and PetrologyUniversity of GöttingenFederal Republic of Germany

Bibliographic information

  • DOI https://doi.org/10.1007/978-1-4757-4215-2
  • Copyright Information Springer-Verlag New York 1979
  • Publisher Name Springer, New York, NY
  • eBook Packages Springer Book Archive
  • Print ISBN 978-0-387-90413-9
  • Online ISBN 978-1-4757-4215-2
  • Series Print ISSN 0172-6234
  • Buy this book on publisher's site