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The Deep Proterozoic Crust in the North Atlantic Provinces

  • Alex C. Tobi
  • Jacques L. R. Touret

Part of the NATO ASI Series book series (ASIC, volume 158)

Table of contents

  1. Front Matter
    Pages i-xv
  2. The Deep Proterozoic Crust in the North-Atlantic Provinces

    1. K. S. Heier
      Pages 1-2
    2. N. J. Vlaar
      Pages 3-20
    3. Scott B. Smithson, William R. Pierson, Sharon L. Wilson, Roy A. Johnson
      Pages 21-37
    4. R. F. Emslie
      Pages 39-60
    5. William M. Lamb, John W. Valley
      Pages 119-131
  3. The Proterozoic Provinces in North America and Greenland

  4. The Proterozoic Provinces in South Scandinavia: Geological Evolution and Structure

  5. The Proterozoic Provinces in South Scandinavia: Geochronology and Geochemistry

  6. Back Matter
    Pages 585-603

About this book

Introduction

The Proterozoic terrains of South Scandinavia and the Grenville Province in North-America have many common features : Regional high­ grade metamorphism (Granulite-facies), anorthosites, etc. They are separated by the Caledonian orogeny and, above all, by the Atlantic Ocean. During the time of the great continental drift controversy, few people were ready to admit that both sides on the Atlantic were once an unique province. Now everybody agrees on the Post-paleozoic age of the Atlantic and, consequently, on the intrinsic homogeneity of the much older. rocks which occur around it. But a detailed comparison is not easy. The Grenville Province is much larger than South Scandinavia, both regions have been investigated by a great number of different schools, using various methods, approaches and concepts. After several attempts, and long discussion, it was felt by a small group of individuals, that literature study would not be enough and that nothing could re­ place the direct contact, in the field, of specialists who had a first­ hand knowledge of all involved regions. The formula of a NATO Advanced Study Institute, which gives a unique opportunity to meet and mix people of various origin and levels, came almost by itself. Much work was needed, much help has been obtained, as detailed in the "Acknowledgements".

Keywords

Cambrian Proterozoic fault fault zone geochronology igneous rock orogenic belt orogeny tectonics

Editors and affiliations

  • Alex C. Tobi
    • 1
  • Jacques L. R. Touret
    • 2
  1. 1.Earth Science InstituteState UniversityUtrechtThe Netherlands
  2. 2.Earth Science InstituteThe Free UniversityAmsterdamThe Netherlands

Bibliographic information

  • DOI https://doi.org/10.1007/978-94-009-5450-2
  • Copyright Information Springer Science+Business Media B.V. 1985
  • Publisher Name Springer, Dordrecht
  • eBook Packages Springer Book Archive
  • Print ISBN 978-94-010-8907-4
  • Online ISBN 978-94-009-5450-2
  • Series Print ISSN 1389-2185
  • Buy this book on publisher's site