Articles | Volume 9, issue 4
https://doi.org/10.5194/se-9-1011-2018
https://doi.org/10.5194/se-9-1011-2018
Research article
 | 
10 Aug 2018
Research article |  | 10 Aug 2018

Non-cylindrical parasitic folding and strain partitioning during the Pan-African Lufilian orogeny in the Chambishi–Nkana Basin, Central African Copperbelt

Koen Torremans, Philippe Muchez, and Manuel Sintubin

Viewed

Total article views: 3,286 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,022 1,123 141 3,286 415 110 118
  • HTML: 2,022
  • PDF: 1,123
  • XML: 141
  • Total: 3,286
  • Supplement: 415
  • BibTeX: 110
  • EndNote: 118
Views and downloads (calculated since 06 Feb 2018)
Cumulative views and downloads (calculated since 06 Feb 2018)

Viewed (geographical distribution)

Total article views: 3,286 (including HTML, PDF, and XML) Thereof 2,926 with geography defined and 360 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 29 Jun 2024
Download
Short summary
A major mountain building event, called the Lufilian orogeny, deformed the rocks that host copper and cobalt ore in the world-class Central African Copperbelt. Key field evidence in this study shows that a single pulse of deformation caused a set of complexly interacting folds and faults. The specific composition and layering in the rock package has a major influence on how the rock sequence was folded.