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Oceanic basalts [Libro electrónico] / edited by P. A. Floyd

Floyd, P. A [editor].
Tipo de material: Libro en línea Libro en línea Editor: New York, New York, United States: Van Nostrand Reinhold, c1991Descripción: xiv, 456 páginas : ilustraciones mapas ; 24 centímetros.ISBN: 9781461365716 (Print); 9781461535409 (Online).Tema(s): Basalt | Ocean bottom | MagmatismNota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía e índice: páginas 398-450 Número de sistema: 55331Contenidos:Mostrar Resumen:
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Oceanic basalts are the most abundant rock type found at the earth's surface, and as such they have been the subject of considerable research, particularly since the concept of sea-floor spreading became widely accepted. This book provides a review of these rocks, first dicussing how we sample the ocean floor and what we know about the structure of the oceanic crust, followed by an overview of the various regional settings (Pacific crust, Atlantic crust, marginal basins, seamounts and islands) and finally examines the main processes (and their interactions) which prevail during the generation and emplacement of oceanic basalt magmas. This is a volume for geologists, geochemists and geophysicists and a source of reference for advanced undergraduate students and postgraduates in these disciplines.

Recurso en línea: http://link.springer.com/openurl?genre=book&isbn=978-1-4613-6571-6
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Incluye bibliografía e índice: páginas 398-450

Chapter 1. Structure.. Chapter 2. Processes.. Chapter 3. Environments.. Chapter 4. Sources.. Index

Disponible para usuarios de ECOSUR con su clave de acceso

Oceanic basalts are the most abundant rock type found at the earth's surface, and as such they have been the subject of considerable research, particularly since the concept of sea-floor spreading became widely accepted. This book provides a review of these rocks, first dicussing how we sample the ocean floor and what we know about the structure of the oceanic crust, followed by an overview of the various regional settings (Pacific crust, Atlantic crust, marginal basins, seamounts and islands) and finally examines the main processes (and their interactions) which prevail during the generation and emplacement of oceanic basalt magmas. This is a volume for geologists, geochemists and geophysicists and a source of reference for advanced undergraduate students and postgraduates in these disciplines. eng

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