- We will send in 10–14 business days.
/images/books/13495201/9786202572781.jpg)
- Author: Rodrigue Fotie Lele
- Publisher: Our Knowledge Publishing
- ISBN-10: 6202572787
- ISBN-13: 9786202572781
- Format: 15.2 x 22.9 x 0.7 cm, minkšti viršeliai
- Language: English
- SAVE -10% with code: EXTRA
Characteristics of basalt aquifers and basement formations (e-book) (used book) | bookbook.eu
Reviews
Description
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.
EXTRA 10 % discount with code: EXTRA
The promotion ends in 23d.08:39:28
The discount code is valid when purchasing from 10 €. Discounts do not stack.
- Author: Rodrigue Fotie Lele
- Publisher: Our Knowledge Publishing
- ISBN-10: 6202572787
- ISBN-13: 9786202572781
- Format: 15.2 x 22.9 x 0.7 cm, minkšti viršeliai
- Language: English English
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.
Reviews