Origin of igneous rocks: the isotopic evidence [Libro electrónico] / autor: Gunter Faure
Por: Faure, Gunter [autor/a].
Tipo de material: Libro en línea Editor: New York, New York, United States: Springer, c2001Descripción: xv, 496 páginas : ilustraciones mapas ; 28 centímetros.ISBN: 3540677720; 9783642087288 (Print); 9783662044742 (Online).Tema(s): Igneous rocksNota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía e índice: páginas 401-456 Número de sistema: 56477Contenidos:Mostrar Resumen:Tipo de ítem | Biblioteca actual | Colección | Signatura | Estado | Fecha de vencimiento | Código de barras |
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Libros | Biblioteca Electrónica Recursos en línea (RE) | Acervo General | Recurso digital | ECO400564778534 |
Incluye bibliografía e índice: páginas 401-456
1. Chemical properties and isotope systematics.. 2. The origin of volcanic rocks in the oceans.. 3. Subduction zones in the oceans.. 4. The compressive margin of the American continents.. 5. Continental flood basalt provinces.. 6. Alkalic igneous rocks on the continents.. 7. Differentiated gabbro intrusives.. 8. Archean greenstone belts and granitic gneisses of north America.. Subject Index
Disponible para usuarios de ECOSUR con su clave de acceso
His book is intended for graduate students of the Earth Sciences who require a T comprehensive examination of the origins of igneous rocks as recorded by the isotope compositions of the strontium, neodymium, lead, and oxygen they contain. Students who have not had a formal course in the systematics of radiogenic isotopes can acquire a basic understanding of this subject by a careful study of Chap. 1. Addi tional information is readily available in a textbook by Faure (1986). The primary purpose of this book is to demonstrate how the isotope composition of Sr, Nd, Pb, and 0 in igneous rocks has been used to shed light on the origin of igneous rocks and hence on the activity of the mantle and on its interactions with the continental and oceanic crust. The presentations are based on the premise that igneous and metamorphic rocks form as a direct consequence of the dynamic processes of the mantle and of the re sulting interactions between the mantle and the crust. Accordingly, Chap. 2 to 6 ex amine specific types of igneous rocks that form in particular tectonic settings. Each of these chapters starts with questions about the properties of the mantle and crust, and about the relation between the tectonic setting and the rock-forming processes that take place in that setting. eng
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