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The Nature and Models of Metamorphism
Buch von Vladimir V. Reverdatto (u. a.)
Sprache: Englisch

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Beschreibung
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 ¿-¿ parameters and ¿-¿-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 ¿-¿ 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.
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 ¿-¿ parameters and ¿-¿-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 ¿-¿ 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.
Über den Autor
Zusammenfassung

Summarizes latest studies in the fields of metamorphism, geothermobarometry and kinetics of mineral reactions

Contains examples of the evolution of metamorphic complexes in Siberia and Central Asia

Expands the idea of metamorphism as an indicator of geodynamics

Inhaltsverzeichnis
Introduction.- The development of ideas about the mineral transformations and the facies of metamorphism.- Mineral geothermobarometry.- The causes, geodynamic factors and models of metamorphism.- Metamorphic processes in the rocks.- Conclusion.
Details
Erscheinungsjahr: 2019
Fachbereich: Petrographie
Genre: Geowissenschaften, Mathematik, Medizin, Naturwissenschaften, Technik
Rubrik: Naturwissenschaften & Technik
Medium: Buch
Inhalt: xv
330 S.
ISBN-13: 9783030030285
ISBN-10: 3030030288
Sprache: Englisch
Herstellernummer: 978-3-030-03028-5
Einband: Gebunden
Autor: Reverdatto, Vladimir V.
Likhanov, Igor I.
Kolobov, Vasiliy Yu
Sheplev, Valentin S
Polyansky, Oleg P.
Auflage: 1st edition 2019
Hersteller: Springer Nature Switzerland
Springer International Publishing
Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, D-69121 Heidelberg, juergen.hartmann@springer.com
Maße: 241 x 160 x 25 mm
Von/Mit: Vladimir V. Reverdatto (u. a.)
Erscheinungsdatum: 14.01.2019
Gewicht: 0,688 kg
Artikel-ID: 114565954
Über den Autor
Zusammenfassung

Summarizes latest studies in the fields of metamorphism, geothermobarometry and kinetics of mineral reactions

Contains examples of the evolution of metamorphic complexes in Siberia and Central Asia

Expands the idea of metamorphism as an indicator of geodynamics

Inhaltsverzeichnis
Introduction.- The development of ideas about the mineral transformations and the facies of metamorphism.- Mineral geothermobarometry.- The causes, geodynamic factors and models of metamorphism.- Metamorphic processes in the rocks.- Conclusion.
Details
Erscheinungsjahr: 2019
Fachbereich: Petrographie
Genre: Geowissenschaften, Mathematik, Medizin, Naturwissenschaften, Technik
Rubrik: Naturwissenschaften & Technik
Medium: Buch
Inhalt: xv
330 S.
ISBN-13: 9783030030285
ISBN-10: 3030030288
Sprache: Englisch
Herstellernummer: 978-3-030-03028-5
Einband: Gebunden
Autor: Reverdatto, Vladimir V.
Likhanov, Igor I.
Kolobov, Vasiliy Yu
Sheplev, Valentin S
Polyansky, Oleg P.
Auflage: 1st edition 2019
Hersteller: Springer Nature Switzerland
Springer International Publishing
Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, D-69121 Heidelberg, juergen.hartmann@springer.com
Maße: 241 x 160 x 25 mm
Von/Mit: Vladimir V. Reverdatto (u. a.)
Erscheinungsdatum: 14.01.2019
Gewicht: 0,688 kg
Artikel-ID: 114565954
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