Brasiliano orogeny

Target entity: Brasiliano orogeny
Context triple: [Pan-African orogeny, hasPart, Brasiliano orogeny]

• A. Andean orogeny
  The Andean orogeny is the long-lasting mountain-building process responsible for creating and uplifting the Andes Mountains along the western margin of South America due to subduction of oceanic plates beneath the continent.
• B. Cadomian orogeny
  The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.
• C. Variscan orogeny
  The Variscan orogeny was a major late Paleozoic mountain-building event in Europe, broadly contemporaneous with the Appalachian orogeny, that resulted from the collision of continental plates during the assembly of the supercontinent Pangaea.
• D. Grenville orogeny
  The Grenville orogeny was a major Precambrian mountain-building event that helped assemble the supercontinent Rodinia and formed the ancient core of parts of North America and other continents.
• E. Brazilian Highlands
  The Brazilian Highlands are an extensive plateau region covering much of eastern, southern, and central Brazil, known for their diverse landscapes, rich biodiversity, and major role in the country’s climate and river systems.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Target entity: Brasiliano orogeny
Target entity description: The Brasiliano orogeny was a major Neoproterozoic mountain-building event in South America associated with the assembly of the supercontinent Gondwana.

• A. Andean orogeny
  The Andean orogeny is the long-lasting mountain-building process responsible for creating and uplifting the Andes Mountains along the western margin of South America due to subduction of oceanic plates beneath the continent.
• B. Cadomian orogeny
  The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.
• C. Variscan orogeny
  The Variscan orogeny was a major late Paleozoic mountain-building event in Europe, broadly contemporaneous with the Appalachian orogeny, that resulted from the collision of continental plates during the assembly of the supercontinent Pangaea.
• D. Grenville orogeny
  The Grenville orogeny was a major Precambrian mountain-building event that helped assemble the supercontinent Rodinia and formed the ancient core of parts of North America and other continents.
• E. Brazilian Highlands
  The Brazilian Highlands are an extensive plateau region covering much of eastern, southern, and central Brazil, known for their diverse landscapes, rich biodiversity, and major role in the country’s climate and river systems.
• F. None of above. chosen