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The Lufilian Arc (or Lufilian Belt) is part of a system of orogenic belts in southern Africa formed during the Pan-African orogeny, a stage in the formation of the Gondwana supercontinent.It extends across eastern Angola, the Katanga Province of the southern Democratic Republic of the Congo and the northwest of Zambia.The arc is about 800 kilometres (500 mi) long. It has global economic importance owing to its rich deposits of copper and cobalt.

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  • Lufilian-Bogen (de)
  • Arc lufilien (fr)
  • Arco Lufiliano (it)
  • Lufilian Arc (en)
rdfs:comment
  • The Lufilian Arc (or Lufilian Belt) is part of a system of orogenic belts in southern Africa formed during the Pan-African orogeny, a stage in the formation of the Gondwana supercontinent.It extends across eastern Angola, the Katanga Province of the southern Democratic Republic of the Congo and the northwest of Zambia.The arc is about 800 kilometres (500 mi) long. It has global economic importance owing to its rich deposits of copper and cobalt. (en)
  • L'arc lufilien (ou ceinture lufilienne) est l'une des ceintures orogéniques d'Afrique australe qui se sont formées durant l'orogenèse panafricaine, une étape de la formation du supercontinent du Gondwana. Il traverse la partie orientale de l'Angola, la province du Katanga en République démocratique du Congo et le nord-ouest de la Zambie. Il fait environ 800 km de longueur. Il présente une grande importance économique car il est riche en cuivre et en cobalt. (fr)
  • L'arco Lufiliano ( o cintura Lufiliana) fa parte del sistema di cinture orogenetiche dell'Africa meridionale che si sono formate durante l'orogenesi Pan-Africana, che rappresentò uno degli stadi che portarono alla formazione del supercontinente Gondwana. L'arco ha una lunghezza di circa 800 km e si estende attraverso la parte orientale dell'Angola, la Provincia del Katanga nella parte meridionale della Repubblica Democratica del Congo, e la parte nordovest dello Zambia. L'arco riveste una notevole importanza economica per i suoi vasti giacimenti di rame e cobalto. (it)
  • Der Lufilian-Bogen oder auch Lufilian-Gürtel ist ein fossiles, deformiertes Sedimentbecken im zentralen südlichen Afrika, in dem niedrig- bis hochgradig metamorphe Sedimentgesteine (Metasedimente) neoproterozoischen Alters mit geringen magmatischen Anteilen enthalten sind. Deformation und Metamorphose erfolgten im Zuge der Pan-Afrikanischen Orogenese im Wesentlichen durch Interaktion zwischen dem Kongo-São-Francisco- und Kalahari-Kraton. Die entsprechende Faltungsphase wird auch Lufilian-Orogenese genannt. (de)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Zambia_3.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Carrollite-Calcite-168081.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Libethenite-tuc1033b.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Spherocobaltite-Dolomite-120467.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Kuunga2.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Anticline_(PSF)-vector.svg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Molten_copper_being_poured_-_MCM_Mufilira.jpg
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