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The Lachlan Fold Belt (LFB) or Lachlan Orogen is a geological subdivision of the east part of Australia. It is a zone of folded and faulted rocks of similar age. It dominates New South Wales and Victoria, also extending into Tasmania, the Australian Capital Territory and Queensland. It was formed in the Middle Paleozoic from 450 to 340 Mya. It was earlier known as Lachlan Geosyncline. It covers an area of 200,000 km2.

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  • Lachlan fold belt (fr)
  • Lachlan Fold Belt (en)
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  • The Lachlan Fold Belt (LFB) or Lachlan Orogen is a geological subdivision of the east part of Australia. It is a zone of folded and faulted rocks of similar age. It dominates New South Wales and Victoria, also extending into Tasmania, the Australian Capital Territory and Queensland. It was formed in the Middle Paleozoic from 450 to 340 Mya. It was earlier known as Lachlan Geosyncline. It covers an area of 200,000 km2. (en)
  • La Lachlan fold belt est une région géologique du sud-est de l'Australie correspondant approximativement au sud-est de la Nouvelle-Galles du Sud et à la majeure partie de l'État de Victoria. D'une superficie d'environ 300 000 km2, cette région a été le siège d'une intense activité volcanique au Silurien et au Devonien ainsi qu'au Carbonifère pour le nord-est de la région. C'est donc une région formée de roches volcaniques et de roches granitiques. (fr)
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  • The Lachlan Fold Belt (LFB) or Lachlan Orogen is a geological subdivision of the east part of Australia. It is a zone of folded and faulted rocks of similar age. It dominates New South Wales and Victoria, also extending into Tasmania, the Australian Capital Territory and Queensland. It was formed in the Middle Paleozoic from 450 to 340 Mya. It was earlier known as Lachlan Geosyncline. It covers an area of 200,000 km2. (en)
  • La Lachlan fold belt est une région géologique du sud-est de l'Australie correspondant approximativement au sud-est de la Nouvelle-Galles du Sud et à la majeure partie de l'État de Victoria. D'une superficie d'environ 300 000 km2, cette région a été le siège d'une intense activité volcanique au Silurien et au Devonien ainsi qu'au Carbonifère pour le nord-est de la région. C'est donc une région formée de roches volcaniques et de roches granitiques. (fr)
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