Arc Volcano of Japan: Generation of Continental Crust from the Mantle: Lecture Notes in Earth Sciences, cartea 136
Autor Takeru Yanagien Limba Engleză Hardback – 7 iul 2011
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Specificații
ISBN-13: 9784431539957
ISBN-10: 4431539956
Pagini: 140
Ilustrații: XI, 123 p.
Dimensiuni: 155 x 235 x 12 mm
Greutate: 0.48 kg
Ediția:2011
Editura: Springer
Colecția Springer
Seria Lecture Notes in Earth Sciences
Locul publicării:Tokyo, Japan
ISBN-10: 4431539956
Pagini: 140
Ilustrații: XI, 123 p.
Dimensiuni: 155 x 235 x 12 mm
Greutate: 0.48 kg
Ediția:2011
Editura: Springer
Colecția Springer
Seria Lecture Notes in Earth Sciences
Locul publicării:Tokyo, Japan
Public țintă
ResearchCuprins
Chapter 1 Continental Crust and Granitic Plutons.- Chapter 2 Chemical Composition of Continental Crust and the Primitive Mantle.- Chapter 3 Origin of Magmas of the Bowen’s Series.- Chapter 4 Search for the Formation Mechanism of Continental Crust.- Chapter 5 Differentiation Mechanism of Magma at Arc Volcanoes.- Chapter 6 Configuration and Dynamics of the Magma Chambers Beneath Arc Volcanoes.- Chapter 7 Island Arc Volcanic Rocks and the Upper Continental Crust.- Chapter 8 Volcanic Arcs and Outer Arcs.
Notă biografică
Professor Emeritus at Kyushu University
Textul de pe ultima copertă
This book presents an analysis of our current knowledge on the origin of the Earth’s continental crust. There are two aspects to consider: tectonic and igneous processes. Tectonic aspects include sedimentary accretion, terrane accretion, and continental collision at continental margins, in association with plate subduction. These processes result in the formation of large mountain belts, the building up of which literally grows the continents. However, these tectonic aspects are concerned with material recycling within the crust, and hence do not contribute to volumetric growth of continental crust. Igneous processes concern separation of continental crust from the mantle and result in the volumetric growth of continental crust. Therefore, the main focus of this book is to systematically examine why and how the Earth’s continental crust forms, by evaluating magmatic processes at island arcs where new continental crust forms.
Caracteristici
Present the discovery of crystallization differentiation in an open-system chamber, repeatedly supplied with primitive magma from the mantle Describe island arc volcanic rocks which represent a range of magmas formed during the evolution of primitive basaltic magma Explain the growth not only of volcanic arc but also of outer arc, as well as the interrelationships between geophysical and geological configurations of island arcs Includes supplementary material: sn.pub/extras