The tropical cratonic geosystem encompasses non-orogenic continental domains of the
tropical belt that developed and preserved Cenozoic lateritic regolith mantles (ie, the …

Abstract The middle Triassic Kani Zarrineh bauxite deposit, in the Irano–Himalayan belt,
located 20 km northwest of Saqqez city in northwestern Iran, occurs in depressions of the …

This book focuses on the definition, distribution, arrangement and formation of the
ferruginous, aluminous or silico-aluminous hydrated or nonhydrated minerals within lateritic …

A simple geochemical balance of lateritization processes governing the development of
several tens of meters of weathering profiles overlain by ferricretes is estimated on the basis …

The Balaya bauxite plateau is located in the Kindia bauxite province; where the bauxite ores
are found above Ordovician and Silurian formations in the southern part of the Guinean …

Formation and transformation processes of iron duricrust developed under tropical humid
conditions in the southeastern part of the Central African Republic have been investigated in …

The laterite deposits occur in a linear stretch along the northern Arabian Sea coast in the
Jamnagar and Porbandar districts of, Gujarat state, India. These deposits are characterised …

In southeastern Central African Republic the lateritic weathering mantles are capped by 2 to
5 m thick ferricretes, which previously formed under a seasonal tropical climate. The actual …

The Arbanos bauxite deposit is located in the Iran-Himalayan karst-type bauxite belt and
about 25 km northeast of Bukan city, northwestern Iran. The bauxite ores occur as layers and …

Petrographical, mineralogical, and geochemical characteristics of a blanket‐type lateritic
bauxite deposit, bordering the Deccan basalt in Kachchh, are investigated to interpret the …