Geotechnical evaluation of rocks and soils in Catoca kimberlitic mining complex (Angola)

Landslides and rock sliding occur very frequently in the mining area of Catoca, located in Angola. Therefore, a physical/mechanical and geotechnical characterization of the massif and the rock matrix was carried out adopting the landslide classifications as proposed by Hutchinson and Varnes. The saf...

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Main Authors: Domingos M. Dos Santos Neves-Margarida, Rafael Guardado-Lacaba
Format: Article
Language:Spanish
Published: Universidad de Moa "Dr. Antonio Núñez Jiménez" 2012-10-01
Series:Minería y Geología
Subjects:
Online Access:http://revista.ismm.edu.cu/index.php/revistamg/article/view/496
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spelling doaj-3c8dd74b15e14b1487dab0bbd4e7f0262020-11-25T00:47:45ZspaUniversidad de Moa "Dr. Antonio Núñez Jiménez"Minería y Geología1993-80122012-10-01283117Geotechnical evaluation of rocks and soils in Catoca kimberlitic mining complex (Angola)Domingos M. Dos Santos Neves-MargaridaRafael Guardado-LacabaLandslides and rock sliding occur very frequently in the mining area of Catoca, located in Angola. Therefore, a physical/mechanical and geotechnical characterization of the massif and the rock matrix was carried out adopting the landslide classifications as proposed by Hutchinson and Varnes. The safety factor was applied based on the structural weakness coefficient (λ); resulting in 0.70 in surface rocks, sandstones and intraformational sands; 0.58 in oversaturated eluvial gneiss; 0.50 in cracked gneiss and 0.47 in the ore compound of weathered, moist kimberlitic porphyric and weathered porphyric kimberlite. These results indicate the low strength of the massif and the need to reformulate the activities in the mine and the construction of more stable slopes. It could also be observed that deformation of rocks in the slopes and the cuts in the Catoca mine is conditioned by the movement of underground water within the rock massif itself.http://revista.ismm.edu.cu/index.php/revistamg/article/view/496Geotechnicskimberlite ore bodieslandslidesslope stability
collection DOAJ
language Spanish
format Article
sources DOAJ
author Domingos M. Dos Santos Neves-Margarida
Rafael Guardado-Lacaba
spellingShingle Domingos M. Dos Santos Neves-Margarida
Rafael Guardado-Lacaba
Geotechnical evaluation of rocks and soils in Catoca kimberlitic mining complex (Angola)
Minería y Geología
Geotechnics
kimberlite ore bodies
landslides
slope stability
author_facet Domingos M. Dos Santos Neves-Margarida
Rafael Guardado-Lacaba
author_sort Domingos M. Dos Santos Neves-Margarida
title Geotechnical evaluation of rocks and soils in Catoca kimberlitic mining complex (Angola)
title_short Geotechnical evaluation of rocks and soils in Catoca kimberlitic mining complex (Angola)
title_full Geotechnical evaluation of rocks and soils in Catoca kimberlitic mining complex (Angola)
title_fullStr Geotechnical evaluation of rocks and soils in Catoca kimberlitic mining complex (Angola)
title_full_unstemmed Geotechnical evaluation of rocks and soils in Catoca kimberlitic mining complex (Angola)
title_sort geotechnical evaluation of rocks and soils in catoca kimberlitic mining complex (angola)
publisher Universidad de Moa "Dr. Antonio Núñez Jiménez"
series Minería y Geología
issn 1993-8012
publishDate 2012-10-01
description Landslides and rock sliding occur very frequently in the mining area of Catoca, located in Angola. Therefore, a physical/mechanical and geotechnical characterization of the massif and the rock matrix was carried out adopting the landslide classifications as proposed by Hutchinson and Varnes. The safety factor was applied based on the structural weakness coefficient (λ); resulting in 0.70 in surface rocks, sandstones and intraformational sands; 0.58 in oversaturated eluvial gneiss; 0.50 in cracked gneiss and 0.47 in the ore compound of weathered, moist kimberlitic porphyric and weathered porphyric kimberlite. These results indicate the low strength of the massif and the need to reformulate the activities in the mine and the construction of more stable slopes. It could also be observed that deformation of rocks in the slopes and the cuts in the Catoca mine is conditioned by the movement of underground water within the rock massif itself.
topic Geotechnics
kimberlite ore bodies
landslides
slope stability
url http://revista.ismm.edu.cu/index.php/revistamg/article/view/496
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