Name: Characteristics of basalt aquifers and basement formations (en Inglés)
SKU: 57604939
Price: 161.33 PEN
Availability: InStock
Author: Fotie Lele, Rodrigue ; Nono, Alexandre ; Temgoua, Emile
ISBN: 9786202572781

portada Characteristics of basalt aquifers and basement formations (en Inglés)

Characteristics of basalt aquifers and basement formations (en Inglés)

Formato

Libro Físico

Autor

Alexandre Nono

Emile Temgoua

Rodrigue Fotie Lele

Editorial

Our Knowledge Publishing

Idioma

Inglés

N° páginas

120

Encuadernación

Tapa Blanda

Dimensiones

22.9x15.2x0.7 cm

Peso

0.19 kg.

ISBN13

9786202572781

Categorías

Ciencias de la tierra/geociencias

Characteristics of basalt aquifers and basement formations (en Inglés)

Alexandre Nono (Autor) · Emile Temgoua (Autor) · Rodrigue Fotie Lele (Autor) · Our Knowledge Publishing · Tapa Blanda

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Reseña del libro "Characteristics of basalt aquifers and basement formations (en Inglés)"

This book presents a comparison of the mineralization of water that has circulated at the contact of basalts and basement formations. The results of the study are derived from morpho-structural, petrographic and hydrogeochemical approaches. The Koutaba sector has a dominance of basalts composed of olivine, clinopyroxene, plagioclase and opaque oxides, put in place through faults of major directions: N10-20 E, N60-70 E and N130-140 E. However, the Bapa sector is dominated by granite composed of biotite, mega crystals of alkaline feldspar, quartz, accessory minerals (apatite and zircon) and oxide, of general structural orientation NE-SW, N30-40 E, N130-140 E.The alkaline (Na, K), alkaline earth (Mg) elements and the total mineralization rate make it possible to differentiate the waters flowing through basalts and granites. The waters on basalt have a geochemical background dominated by Ca-Mg-Na-HCO3-SO4 with a relatively high total mineralization while the waters on granite are dominated by Ca-Na-K-HCO3-SO4 in addition to being characterized by low mineralization.