Le livre est actuellement en rupture de stock
En savoir plus sur le livre
Bauxites in permanently uplifted continental areas („Uplift bauxites“). They were formed above the ground-water table and therefore are characterized by a good descendent drainage during weathering under oxic conditions, by epigenetic degradation, erosion and younger soil overprint, and by a low iron mobilisation and saprolite formation. They are generally red. Such bauxites have never before been described under this point of view. The main bauxite „event“ occurred world-wide during the time interval from Upper Cretaceous to Middle Eocene. This phenomenon is exemplified by occurrences in Brazil.
Achat du livre
The tertiary bauxite belt on tectonic uplift areas in the Serra da Mantiqueira, South-East Brazil, Ida Valeton
- Langue
- Année de publication
- 1991
Nous vous informerons par e-mail dès que nous l’aurons retrouvé.
Modes de paiement
Personne n'a encore évalué .