Name: Magmatic Sulfide Deposits: Geology, Geochemistry and Exploration (en Inglés)
Price: 1504357.00 COP
Availability: InStock
Author: Anthony Naldrett
ISBN: 9783642060991

portada Magmatic Sulfide Deposits: Geology, Geochemistry and Exploration (en Inglés)

Formato

Libro Físico

Editorial

Springer

Autor

Anthony Naldrett

Año

2010

Idioma

Inglés

N° páginas

728

Encuadernación

Tapa Blanda

ISBN

3642060994

ISBN13

9783642060991

N° edición

Categorías

Geología, geomorfología y litosfera

Magmatic Sulfide Deposits: Geology, Geochemistry and Exploration (en Inglés)

Anthony Naldrett (Autor) · Springer · Tapa Blanda

Libro Nuevo

$ 1.504.357

$ 2.507.261

Ahorras: $ 1.002.904

40% descuento

Envío normal

Origen: Estados Unidos (Costos de importación incluídos en el precio)

Se enviará desde nuestra bodega entre el Lunes 20 de Mayo y el Lunes 03 de Junio.

Lo recibirás en cualquier lugar de Colombia entre 1 y 5 días hábiles luego del envío.

Reseña del libro "Magmatic Sulfide Deposits: Geology, Geochemistry and Exploration (en Inglés)"

PGE V-Voisey's Bay (Canada) D -Duluth Complex (USA) K-Kambalda (Australia) M-Merensky Reef (Bushveld) N -Noril'sk region (Russia) P-Pechenga(Russia) S-Sudbury (Canada) T-Thompson (Canada) J -Jinchuan (China) L-Lac des lies (Canada) PR-Platreef (Bushveld) Po-Portimo Complex (Finland) R-Raglan (Canada) U-UG-2 chromitite (Bushveld) Z-Great Dyke of Zimbabwe e-Mt Keith (Australia) . ä. -Perseverance (Australia) +-Stillwater (USA) 0 0 0 'c9 -~ Ni+Co Cu Relative value of Ni+Co Fig. 1. 1. Relative va1ue of the contributions of Ni+Co, Cu and PGE to the mag matic su1fide deposits listed in Table 1. 1 sulfide deposits are closely related to bodies of mafic or ultramafic rock, and the most convenient way in which to consider them is in terms of the type of magma responsible for the rocks with which they are associated. Typically the type of magma involved bears a close relationship to the tec tonic setting within which it was emplaced. The locations of important deposits, both Ni-Cu dominant and PGE dominant, are shown in Fig. 1. 2. Considering first Ni-Cu deposits, these are further divided into six classes (Table 1. 2) on the basis of their associated magma type. Class NC- 1 (Chap. 3) comprises those related to komatiitic magmatism. Currently known deposits fall into two sub-classes, those related to Archean komatiites ( e. g. the deposits of Western Australia, Zimbabwe and the Abitibi belt of Canada) and those related to Proterozoic komatiites (e. g. those ofthe Raglau and Thompson belts which arebothin Canada)l.