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The Nature and Models of Metamorphism

  • Vladimir V.  Reverdatto
  • Igor I. Likhanov
  • Oleg P. Polyansky
  • Valentin S Sheplev
  • Vasiliy Yu Kolobov

Part of the Springer Geology book series (SPRINGERGEOL)

Table of contents

  1. Front Matter
    Pages i-xv
  2. Vladimir V. Reverdatto, Igor I. Likhanov, Oleg P. Polyansky, Valentin S. Sheplev, Vasiliy Yu. Kolobov
    Pages 1-54
  3. Vladimir V. Reverdatto, Igor I. Likhanov, Oleg P. Polyansky, Valentin S. Sheplev, Vasiliy Yu. Kolobov
    Pages 55-82
  4. Vladimir V. Reverdatto, Igor I. Likhanov, Oleg P. Polyansky, Valentin S. Sheplev, Vasiliy Yu. Kolobov
    Pages 83-228
  5. Vladimir V. Reverdatto, Igor I. Likhanov, Oleg P. Polyansky, Valentin S. Sheplev, Vasiliy Yu. Kolobov
    Pages 229-328
  6. Back Matter
    Pages 329-330

About this book

Introduction

This book presents the genetic connections of metamorphism and geodynamics. It discusses the tectonic and magmatic processes as the reason of metamorphism, and the geological types of metamorphism, which define the features of Р-Т parameters and Р-Т-t paths. Three categories of metamorphism are distinguished depending on the heat flow rate: 1) at a geothermal gradient near to an average terrestrial ("normal") value; 2) at a heightened thermal gradient as the result of additional heat supply in the earth's crust by magmatic intrusions and diapirism of magma; 3) at a reduced thermal gradient during the collision of lithosphere plates and blocks of the earth's crust.  The quantitative methods of description of metamorphism have been widely used in this book. The mathematical models of metamorphism have been studied in connection with magmatic intrusions, rifting process and magmatic diapirism. Mineral changes in the rocks controlled by variations of Р-Т of parameters, mass transfer and chemical reactions have also been characterized. The book proposes a quasi-stationary model of diffusion metasomatism with respect to the formation of zonal structures of minerals. The method of mineral thermobarometry for the conditions of unsteady equilibrium has been worked out; the quantitative analysis of mass transfer during metamorphic reactions in the rock matrix has been carried out, and the mobility of chemical elements at metamorphism has been estimated as well. 

The book is intended for specialists in the fields of petrology, mineralogy and geochemistry, and for students at the senior and graduate level.

Keywords

p-T paths diapirism Thermobarometry Geodynamics Korzhinsky-Fisher-Joesten model Kinetics of metamorphic reactions Mathematical models of metamorphism interpretation of metamorphic processes Observation of metamorphic processes metamorphic mineralogy metamorphic petrology metamorphic geochemistry Geothermobarometry

Authors and affiliations

  • Vladimir V.  Reverdatto
    • 1
  • Igor I. Likhanov
    • 2
  • Oleg P. Polyansky
    • 3
  • Valentin S Sheplev
    • 4
  • Vasiliy Yu Kolobov
    • 5
  1. 1.V.S. Sobolev Institute of Geology and GeophysicsSiberian Branch, Russian Academy of SciencesNovosibirskRussia
  2. 2.V.S. Sobolev Institute of Geology and GeophysicsSiberian Branch, Russian Academy of SciencesNovosibirskRussia
  3. 3.V.S. Sobolev Institute of Geology and GeophysicsSiberian Branch, Russian Academy of SciencesNovosibirskRussia
  4. 4.V.S. Sobolev Institute of Geology and GeophysicsSiberian Branch, Russian Academy of SciencesNovosibirskRussia
  5. 5.V.S. Sobolev Institute of Geology and GeophysicsSiberian Branch, Russian Academy of SciencesNovosibirskRussia

Bibliographic information

  • DOI https://doi.org/10.1007/978-3-030-03029-2
  • Copyright Information Springer Nature Switzerland AG 2019
  • Publisher Name Springer, Cham
  • eBook Packages Earth and Environmental Science
  • Print ISBN 978-3-030-03028-5
  • Online ISBN 978-3-030-03029-2
  • Series Print ISSN 2197-9545
  • Series Online ISSN 2197-9553
  • Buy this book on publisher's site
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