Plate Tectonics [recurso electrónico] : Continental Drift and Mountain Building / by Wolfgang Frisch, Martin Meschede, Ronald C. Blakey.
Tipo de material: TextoEditor: Berlin, Heidelberg : Springer Berlin Heidelberg, 2011Descripción: VIII, 212 p. online resourceTipo de contenido: text Tipo de medio: computer Tipo de portador: online resourceISBN: 9783540765042Tema(s): Geography | Geology | Geology, Structural | Planetology | Earth Sciences | Geology | Structural Geology | PlanetologyFormatos físicos adicionales: Printed edition:: Sin títuloClasificación CDD: 551 Clasificación LoC:QE1-996.5Recursos en línea: Libro electrónico En: Springer eBooksResumen: How are mountains formed? Why are there old and young mountains? Why do the shapes of South America and Africa fit so well together? Why is the Pacific surrounded by a ring of volcanoes and earthquake-prone areas while the edges of the Atlantic are relatively peaceful? Frisch and Meschede and Blakey answer all these questions and more through the presentation and explanation of the geodynamic processes upon which the theory of continental drift is based and which have led to the concept of plate tectonics.Tipo de ítem | Biblioteca actual | Colección | Signatura | Copia número | Estado | Fecha de vencimiento | Código de barras |
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Libro Electrónico | Biblioteca Electrónica | Colección de Libros Electrónicos | QE1 -996.5 (Browse shelf(Abre debajo)) | 1 | No para préstamo | 373212-2001 |
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QD453 .L665 2014 EB Principios de fisicoquímica | QD75 C555 2009 EB Química analítica | QE1 -996.5 Petrogenesis of Metamorphic Rocks | QE1 -996.5 Plate Tectonics | QE1 -996.5 The Mjølnir Impact Event and its Consequences | QE1 -996.5 Arc-Continent Collision | QE1 -996.5 Cratons and Fold Belts of India |
How are mountains formed? Why are there old and young mountains? Why do the shapes of South America and Africa fit so well together? Why is the Pacific surrounded by a ring of volcanoes and earthquake-prone areas while the edges of the Atlantic are relatively peaceful? Frisch and Meschede and Blakey answer all these questions and more through the presentation and explanation of the geodynamic processes upon which the theory of continental drift is based and which have led to the concept of plate tectonics.
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