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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Universidad de Moa "Dr. Antonio Núñez Jiménez"
2012-10-01
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Online Access: | http://revista.ismm.edu.cu/index.php/revistamg/article/view/496 |
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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 |
work_keys_str_mv |
AT domingosmdossantosnevesmargarida geotechnicalevaluationofrocksandsoilsincatocakimberliticminingcomplexangola AT rafaelguardadolacaba geotechnicalevaluationofrocksandsoilsincatocakimberliticminingcomplexangola |
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