Add to ORKGInternational audienceThe Brazilian Central Plateau Latosols occurs on Tertiary South American and Velhas planning surfaces. The purpose of this work was to determine activation energy of kaolinite dehydroxylation and its genesis relationships of the Brazilian Central Plateau Latosols
The tropical weathering of sedimentary kaolin deposits from the plateaux surrounding Manaus (Alter d...
The Capim River kaolin, located in the eastern Brazilian Amazon, constitutes one of the most importa...
O caolim da Bacia de Campo Alegre, Estado de Santa Catarina, Brasil, formou-se da alteração de rocha...
planning surfaces. The purpose of this work was to determine activation energy of kaolinite dehydrox...
International audienceThe Brazilian Central Plateau is constituted of the South American Surface and...
The Brazilian Central Plateau is constituted of the two main geomorphic surfaces: the South American...
Latosols are deeply weathered soils characteristic of the moist tropics. Many Latosols have kaolinit...
Les Latosols correspondent à environ 40% du Plateau Central brésilien. Ils sont caractérisés par une...
The mineralogy of the Latosols of the Brazilian Central Plateau remains under discussion in the abse...
The Latosols correspond to about 40% of the Brazilian Central Plateau. They are characterized by low...
Latosols are deeply weathered soils characteristic of the moist tropics. Many Latosols have kaolinit...
Red kaolinite (RK) with isomorphic iron originating from kaolinic clays from Campos Sales region loc...
International audienceThe tropical weathering of sedimentary kaolin deposits from the plateaux surro...
The Latosols correspond to about 40% of the Brazilian Central Plateau. They are characterized by low...
The tropical weathering of sedimentary kaolin deposits from the plateaux surrounding Manaus (Alter d...
The tropical weathering of sedimentary kaolin deposits from the plateaux surrounding Manaus (Alter d...
The Capim River kaolin, located in the eastern Brazilian Amazon, constitutes one of the most importa...
O caolim da Bacia de Campo Alegre, Estado de Santa Catarina, Brasil, formou-se da alteração de rocha...
planning surfaces. The purpose of this work was to determine activation energy of kaolinite dehydrox...
International audienceThe Brazilian Central Plateau is constituted of the South American Surface and...
The Brazilian Central Plateau is constituted of the two main geomorphic surfaces: the South American...
Latosols are deeply weathered soils characteristic of the moist tropics. Many Latosols have kaolinit...
Les Latosols correspondent à environ 40% du Plateau Central brésilien. Ils sont caractérisés par une...
The mineralogy of the Latosols of the Brazilian Central Plateau remains under discussion in the abse...
The Latosols correspond to about 40% of the Brazilian Central Plateau. They are characterized by low...
Latosols are deeply weathered soils characteristic of the moist tropics. Many Latosols have kaolinit...
Red kaolinite (RK) with isomorphic iron originating from kaolinic clays from Campos Sales region loc...
International audienceThe tropical weathering of sedimentary kaolin deposits from the plateaux surro...
The Latosols correspond to about 40% of the Brazilian Central Plateau. They are characterized by low...
The tropical weathering of sedimentary kaolin deposits from the plateaux surrounding Manaus (Alter d...
The tropical weathering of sedimentary kaolin deposits from the plateaux surrounding Manaus (Alter d...
The Capim River kaolin, located in the eastern Brazilian Amazon, constitutes one of the most importa...
O caolim da Bacia de Campo Alegre, Estado de Santa Catarina, Brasil, formou-se da alteração de rocha...