Geology of Ore Deposits

, 53:295

The Catoca kimberlite pipe, Republic of Angola: A paleovolcanological model

  • V. A. Pervov
  • S. V. Somov
  • A. V. Korshunov
  • E. V. Dulapchii
  • J. T. Félix
Article

DOI: 10.1134/S1075701511040052

Cite this article as:
Pervov, V.A., Somov, S.V., Korshunov, A.V. et al. Geol. Ore Deposits (2011) 53: 295. doi:10.1134/S1075701511040052

Abstract

The Catoca kimberlite pipe is among the world’s largest primary diamond deposits. The Catoca volcanic edifice is only slightly eroded. Kimberlitic rocks of various facies compose a crater of about 1 km in diameter and a diatreme. The structure of the pipe and mining conditions of the deposit are complicated by intense intrapipe tectonic processes related to large-amplitude subsidence. Based on geological data, we propose a structural model of the deposit and a paleovolcanological model of the Catoca pipe formed during a full cycle beginning with a stage of active volcanism and completed by stages of gradually waning volcanic activity and sedimentation. It is suggested that the banded tuffisitic kimberlite of the crater zone was deposited at the stage of active volcanic eruption from specific pyroclastic suspension as a low-viscosity mixture of crystals and aqueous sol rich in serpentine.

Copyright information

© Pleiades Publishing, Ltd. 2011

Authors and Affiliations

  • V. A. Pervov
    • 1
  • S. V. Somov
    • 1
  • A. V. Korshunov
    • 1
  • E. V. Dulapchii
    • 1
  • J. T. Félix
    • 1
  1. 1.Departamento de Geologia, Sociedade Mineira de CatocaRepública de AngolaLunda Sul, CatocaAngola