Granitoid Rocks
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Author | : D.B. Clarke |
Publisher | : Springer Science & Business Media |
Total Pages | : 302 |
Release | : 1992-05-31 |
Genre | : Science |
ISBN | : 9780412291708 |
By stressing the various techniques used to determine the petrogenic history of granites, and by bridging the gap between undergraduate and research texts, this book provides a clear understanding of the current state of knowledge of the granite family.
Author | : Bernard Barbarin |
Publisher | : |
Total Pages | : 36 |
Release | : 1989 |
Genre | : Geology |
ISBN | : |
Author | : Kurt Bucher |
Publisher | : Springer Science & Business Media |
Total Pages | : 298 |
Release | : 2013-04-17 |
Genre | : Science |
ISBN | : 3662030004 |
Metamorphic rocks are one of the three classes of rocks. Seen on a global scale they constitute the dominant material of the Earth. The understanding of the petrogenesis and significance of metamorphic of geological education. rocks is, therefore, a fundamental topic There are, of course, many different possible ways to lecture on this theme. This book addresses rock metamorphism from a relatively pragmatic view point. It has been written for the senior undergrad uate or graduate student who needs practical knowledge of how to interpret various groups of minerals found in metamorphic rocks. The book is also of interest for the non-specialist and non-petrolo gist professional who is interested in learning more about the geolo gical messages that metamorphic mineral assemblages are sending, as well as pressure and temperature conditions of formation. The book is organized into two parts. The first part introduces the different types of metamorphism, defines some names, terms and graphs used to describe metamorphic rocks, and discusses principal aspects of metamorphic processes. Part I introduces the causes of metamorphism on various scales in time and space, and some principles of chemical reactions in rocks that accompany metamorphism, but without treating these principles in detail, and presenting the thermodynamic basis for quantitative analysis of reactions and their equilibria in metamorphism. Part I also presents concepts of metamorphic grade or intensity of metamorphism, such as the metamorphic-facies concept.
Author | : V. Janoušek |
Publisher | : Geological Society of London |
Total Pages | : 298 |
Release | : 2020-07-02 |
Genre | : Science |
ISBN | : 1786204487 |
Granites (sensu lato) represent the dominant rock-type forming the upper–middle continental crust but their origin remains a matter of long-standing controversy. The granites may result from fractionation of mantle-derived basaltic magmas, or partial melting of different crustal protoliths at contrasting P–T conditions, either water-fluxed or fluid-absent. Consequently, many different mechanisms have been proposed to explain the compositional variability of granites ranging from whole igneous suites down to mineral scale. This book presents an overview of the state of the art, and envisages future avenues towards a better understanding of granite petrogenesis. Particular emphasis of this Volume is on the following topics: Compositional variability of granitic rocks generated in contrasting geodynamic settings during Proterozoic to Phanerozoic Periods, Main permissible mechanisms producing subduction-related granites, Crustal anatexis of different protoliths, and the role of water in granite petrogenesis, New theoretical and analytical tools available for modelling whole-rock geochemistry, in order to decipher the sources and evolution of granitic suites.
Author | : W. K. Witt |
Publisher | : |
Total Pages | : 160 |
Release | : 1997 |
Genre | : Geochemistry |
ISBN | : |
Author | : J. A. Roddick |
Publisher | : Geological Society of America |
Total Pages | : 325 |
Release | : 1983 |
Genre | : Igneous rocks |
ISBN | : 0813711592 |
Author | : J.-L. Bouchez |
Publisher | : Springer Science & Business Media |
Total Pages | : 356 |
Release | : 2013-11-11 |
Genre | : Science |
ISBN | : 9401717176 |
viii debate of those earlier days has been beautifully summarized by H. H. Read in his famous "Granite Controversy" (1957). Read's formulation of the controversy occurred at the time when geochemistry was as a new and powerful tool. The new techniques opened era during which emerging an granites were considered mainly from this new viewpoint. Geochemical signatures have shown that mantle and crustal origins for granites were both possible, but the debate on how and why granites are emplaced did not progress much. Meanwhile, structural geology was essentially geometrical and mechanistic. In the early 70's, the structural approach began to widen to include solid state physics and fluid dynamics. Detailed structural maps of granitic bodies were again published, mainly in France, and analysed in terms of magmatic and plastic flow. The senior editor of this volume and his students deserve much of the credit for this new development. Via microstructural and petrofabric studies, they were able to discriminate between strain in the presence of residual melt or in the solid-state, and, by systematically measuring magnetic fabrics (AMS), they have been able to map magmatic foliations and lineations in ever finer detail, using the internal markers within granites coming from different tectonic environments. The traditional debate has been shifted anew. The burning question now seems to be how the necessary, large-scale or local, crustal extension required for granite emplacement can be obtained.
Author | : B. C. Hearn |
Publisher | : |
Total Pages | : 382 |
Release | : 1983 |
Genre | : Garnet |
ISBN | : |
Author | : Henry Woodward |
Publisher | : |
Total Pages | : 684 |
Release | : 1890 |
Genre | : Geology |
ISBN | : |
Author | : Kurt Bucher |
Publisher | : Springer Science & Business Media |
Total Pages | : 368 |
Release | : 2002 |
Genre | : Science |
ISBN | : 9783540431305 |
Metamorphic rocks make up the largest volume of the Earth. They systematically change their mineralogical composition as a result of tecto-thermal events. The outstanding feature of the 7th edition of this book is the large number of phase diagrams showing the stability relations among minerals and groups of minerals found in metamorphic rocks. The diagrams help to determine the pressure and temperature conditions under which a given collected set of metamorphic rocks may have formed. More than half of the chapters have been completely rewritten or revised. All figures have been edited and improved and recent advances in the field such as multiequilibria thermobarometry and pseudosections were incorporated in the text. The bibliography has been revised and extended, new research publications have also been included. Graduate students will find in depth information on the origin, significance and genesis of metamorphic rocks.