Geological data on the Nyamukubi mining polygon,

Name: Geological data on the Nyamukubi mining polygon,
Brand: Our Knowledge Publishing
SKU: 9786203786590
Price: 34.68 EUR
Availability: InStock

Автор: Bonheur N. Rugain, Ars?ne T. Sadiki

Език:

Корици: С меки корици

Издател: Our Knowledge Publishing

Наличност: Външен склад

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34.68 € 67.82 лв

A geological study of the Kalehe Kibaran (Kivu Supergroup) was carried out using a cartographic, pet...

Информация за книгата

Автор

Bonheur N. Rugain, Ars?ne T. Sadiki

Език

Английски език

Корици

Книга - С меки корици

Издадена

2021

страници

EAN

9786203786590

ISBN

6203786594

Enbook ID

36673940

Издател

Our Knowledge Publishing

Теглоt

Размери

150 x 220 x 3

Пълно описание

A geological study of the Kalehe Kibaran (Kivu Supergroup) was carried out using a cartographic, petrographic, structural and geological approach in the Nyamukubi mining polygon in Kalehe territory. We present the different geological formations outcropping there as well as the different planar and linear structures that have affected them; the results of LPNA and LPA analysis of target samples, prepared and analysed in the laboratory of the Bukavu geological museum and the BGR. Field observations and analyses show an outcrop of metasediments, granitic rocks and intermediate rocks within which quartz veins are observed in abundance in directions parallel to the layers and in certain places, these quartz veins are multidirectional. The structural analysis also shows a schistosity parallel to the stratification planes; two phases of deformations: (D1) compressive, responsible for the formation of the folds and (D2) brittle, which would be responsible for the emplacement of the mineralizations. A geological study of the Kalehe Kibaran (Kivu Supergroup) was carried out using a cartographic, petrographic, structural and geological approach in the Nyamukubi mining polygon in Kalehe territory. We present the different geological formations outcropping there as well as the different planar and linear structures that have affected them; the results of LPNA and LPA analysis of target samples, prepared and analysed in the laboratory of the Bukavu geological museum and the BGR. Field observations and analyses show an outcrop of metasediments, granitic rocks and intermediate rocks within which quartz veins are observed in abundance in directions parallel to the layers and in certain places, these quartz veins are multidirectional. The structural analysis also shows a schistosity parallel to the stratification planes; two phases of deformations: (D1) compressive, responsible for the formation of the folds and (D2) brittle, which would be responsible for the emplacement of the mineralizations.

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