Name: landmark papers: granite petrogenesis (en Inglés)
Price: 251.30 PEN
Availability: InStock
Author: Clemens, John D. ; Bea, Fernando
ISBN: 9780903056304

portada landmark papers: granite petrogenesis (en Inglés)

Formato

Libro Físico

Ilustrado por

John D. Clemens

Fernando Bea

Editorial

Mineralogical Society

Autor

Clemens, John D. ; Bea, Fernando

Año

2012

Idioma

Inglés

N° páginas

356

Encuadernación

Tapa Blanda

Dimensiones

29.7 x 21.0 x 1.9 cm

Peso

0.84 kg.

ISBN

0903056305

ISBN13

9780903056304

Categorías

Geología, geomorfología y litosfera
Rocas, minerales y fósiles

landmark papers: granite petrogenesis (en Inglés)

John D. Clemens (Ilustrado por) · Fernando Bea (Ilustrado por) · Mineralogical Society · Tapa Blanda

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Reseña del libro "landmark papers: granite petrogenesis (en Inglés)"

A compilation of landmark papers on granite petrogenesis is overdue. This volume is organized into a number of sections that represent what the editors regard as the main research fields in which progress has been made in understanding granites and their genesis. The origin of granitic magmas is part of the cycle that unites tectonic processes with the generation of mantle magma, crustal growth, the transfer of mantle heat to the crust, high-grade regional metamorphism, crustal melting and crustal differentiation. The extended subject area is far too wide to deal with in a single volume and therefore the selection has been limited to papers dealing with the formation, physical behaviour and chemical evolution of granitic magmas, and just touching on the matter of associated ore deposits. John (JC) Clemens and Fernando Bea are world experts on the subject of granite petrogenesis. Clemens' most important work has been on the origin and evolution of granites and silicic volcanic magmas, experimental studies and modelling of partial melting and the ascent and chemical evolution of granitic magmas, and these continue to be his main interests. Bea's research interests have been in the petrology and geochemistry of granite rocks and the mechanisms of generation of granite magmas, having studied in detail the role of heat-producing elements.