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Clays in crustal environments: isotope dating and tracing [Libro electrónico] / autores: Norbert Clauer, Sambhu Chaudhuri

Por: Clauer, Norbert [autor/a].
Chaudhuri, Sambhu [autor/a].
Tipo de material: Libro
 en línea Libro en línea Editor: New York, New York, United States: Springer-Verlag, c1995Descripción: xii, 359 páginas : ilustraciones mapas ; 25 centímetros.ISBN: 3540581510; 0387581510; 9783642790874 (Print); 9783642790850 (Online).Tema(s): Clay minerals | Isotope geologyNota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía e índice: páginas 325-354 Número de sistema: 56217Contenidos:Mostrar Resumen:
Inglés

Clay minerals form in a wide variety of crustal environments, e.g. in soil profiles, in sediments at the surface and in deeply buried sedimentary deposits, and under regional, contact and hydrothermal metamorphism conditions. The book provides information about the dynamics of isotope systems in clays and helps us to understand the physical and chemical parameters in the transfer of masses within the crustal domain. Written for graduate students taking courses in sedimentary geochemistry, clay mineralogy, and soil mineralogy, the book will also appeal to scientists carrying out research on clay genesis and mass transfer in crustal environments.

Recurso en línea: http://link.springer.com/openurl?genre=book&isbn=978-3-642-79087-4
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Incluye bibliografía e índice: páginas 325-354

1. An introduction to clay minerals and isotope geochemistry.. 2. Isotope geochemistry of clay minerals in continental weathering environments.. 3. Isotope geochemistry of clay minerals in young continental and oceanic sediments.. 4. Isotope geochemistry of clays and clay minerals from sedimentary rocks.. 5. Isotope geochemistry of mica-type minerals from low-temperature metamorphic rocks.. 6. The frontiers of clay isotope geochemistry.. Subject Index

Disponible para usuarios de ECOSUR con su clave de acceso

Clay minerals form in a wide variety of crustal environments, e.g. in soil profiles, in sediments at the surface and in deeply buried sedimentary deposits, and under regional, contact and hydrothermal metamorphism conditions. The book provides information about the dynamics of isotope systems in clays and helps us to understand the physical and chemical parameters in the transfer of masses within the crustal domain. Written for graduate students taking courses in sedimentary geochemistry, clay mineralogy, and soil mineralogy, the book will also appeal to scientists carrying out research on clay genesis and mass transfer in crustal environments. eng

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