Name: Ber die Vulkanischen Gesteine in Sicilien und Island und Ihre Submarine Umbildung (Cambridge Library Collection - Earth Science) (en Alemán)
Price: 93050.00 CLP
Availability: InStock
Author: Wolfgang Sartorius Von Waltershausen
ISBN: 9781108049504

portada Ber die Vulkanischen Gesteine in Sicilien und Island und Ihre Submarine Umbildung (Cambridge Library Collection - Earth Science) (en Alemán)

Formato

Libro Físico

Editorial

Cambridge University Press

Autor

Wolfgang Sartorius Von Waltershausen

Año

2012

Idioma

Alemán

N° páginas

620

Encuadernación

Tapa Blanda

ISBN

1108049508

ISBN13

9781108049504

Categorías

Química de los minerales, mineralogía y gemas

Ber die Vulkanischen Gesteine in Sicilien und Island und Ihre Submarine Umbildung (Cambridge Library Collection - Earth Science) (en Alemán)

Wolfgang Sartorius Von Waltershausen (Autor) · Cambridge University Press · Tapa Blanda

Libro Nuevo

$ 93.050

$ 143.160

Ahorras: $ 50.110

35% descuento

Envío normal

Origen: España (Costos de importación incluídos en el precio)

Se enviará desde nuestra bodega entre el Miércoles 22 de Mayo y el Miércoles 29 de Mayo.

Lo recibirás en cualquier lugar de Chile entre 1 y 3 días hábiles luego del envío.

Reseña del libro "Ber die Vulkanischen Gesteine in Sicilien und Island und Ihre Submarine Umbildung (Cambridge Library Collection - Earth Science) (en Alemán)"

This mineralogical study, published in 1853 by Darwin's German contemporary Wolfgang Sartorius von Waltershausen (1809-76) illustrates the author's dedication to interdisciplinary research and his desire for greater scientific rigour in geology. Seeking to understand the formation of palagonite, a mineral commonly found in rocks produced by submarine eruptions, Waltershausen realised he would also need to understand the precise composition of another class of minerals, the feldspars, on which Robert Bunsen, also at Göttingen, was working independently. Building on his earlier fieldwork, Waltershausen here reports detailed chemical analyses of minerals from olivine to titanium-iron oxides, dividing rocks into five types according to the proportion of oxygen they contain. He compares palagonites from Iceland and Sicily, and explains the role of erupted ash in producing volcanic edifices. His investigations allow him to propose a detailed model of metamorphic processes, taking into account such factors as pressure, temperature and presence of water.