Name: The Ecology of Areas with Serpentinized Rocks: A World View (en Inglés)
SKU: 56794636
Price: 1004.30 MXN
Availability: InStock
Author: Roberts, B. a. ; Proctor, J.
ISBN: 9789401056540

portada The Ecology of Areas with Serpentinized Rocks: A World View (en Inglés)

The Ecology of Areas with Serpentinized Rocks: A World View (en Inglés)

Formato

Libro Físico

Editorial

Springer

Autor

Roberts, B. a. ; Proctor, J.

Idioma

Inglés

N° páginas

429

Encuadernación

Tapa Blanda

Dimensiones

27.9x21x2.3 cm

Peso

0.99 kg.

ISBN13

9789401056540

Categorías

Botánica y ciencias de las plantas
Ciencia, ingeniería y tecnología medioambientales
Árboles, flores silvestres y plantas: interés general

The Ecology of Areas with Serpentinized Rocks: A World View (en Inglés)

Roberts, B. A. ; Proctor, J. (Autor) · Springer · Tapa Blanda

Libro Nuevo Importado

Envío: 24 a 29 días háb.

$ 2,008.59$ 1,004.30

-50%

Costos de importación incluídos en el precio ✅

Libro Nuevo

Quedan 100 unidades

$ 1,004.30

¡Envío Gratis! Llega entre el 15 Oct y el 23 Oct a CUAUHTÉMOC, Ciudad de México. Seleccionar ubicación

Agregar a lista de deseos

Reseña del libro "The Ecology of Areas with Serpentinized Rocks: A World View (en Inglés)"

B. A. ROBERTS&J. PROCTOR The term 'serpentine' referring to rocks and min- of each of the polymorphs. These conditions in- erals, can be traced back to the ancient Roman clude temperatures of generally less than 530 C, era of Dioscorides (A. D. 50) (Faust & Fahey and fluid pH's in excess of 10 with low pC02- Serpentine protoliths are essentially ultramafic 1962) and they suggest that the speckled colour of serpents and the fact that Dioscorides recom- rocks which fall into a number of categories: (a) mended it for the prevention of snakebite as two stratiform complexes, (b) concentrically zoned complexes, (c) ophiolite complexes and, (d) high- of many origins of the name. It is well known that the use of serpentinized rocks by sculptors temperature peridotite complexes. The most and carvers since ancient times is a tradition that commonly recognized are generally assigned to the ophiolite suite (Malpas, Ch. 2, this is still carried on today (Fig. 1). The differences in chemical composition of serpentinized rocks volume) and occur in most fold-mountain belts are many and specimens come in a wide range of of the world. Serpentinized ultramafic rocks attractive solid and mixed colours, e. g., red, H4(MgFe hSi20 9, approximate composition) green, blue and black.