Scandinavian Caledonides

Target entity: Scandinavian Caledonides
Context triple: [Greenland Caledonides, correlatesWith, Scandinavian Caledonides]

• A. Greenland Caledonides
  The Greenland Caledonides are a major mountain belt in eastern Greenland formed by Paleozoic continental collisions that were part of the broader Caledonian orogenic system spanning present-day North America and Europe.
• B. Sveconorwegian orogeny
  The Sveconorwegian orogeny was a major Mesoproterozoic mountain-building event that shaped much of southwestern Scandinavia, forming part of the ancient basement rocks of the Fennoscandian region.
• 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. Svecofennian orogeny
  The Svecofennian orogeny was a major Paleoproterozoic mountain-building event that formed much of the continental crust of present-day Sweden and Finland within the Fennoscandian Shield.
• E. Karelian orogeny
  The Karelian orogeny was an ancient Paleoproterozoic mountain-building event that shaped much of the bedrock and geological structure of the Fennoscandian Shield in northern Europe.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Target entity: Scandinavian Caledonides
Target entity description: The Scandinavian Caledonides are a major Paleozoic mountain belt in Scandinavia formed by the collision of ancient continental plates during the Caledonian orogeny.

• A. Greenland Caledonides
  The Greenland Caledonides are a major mountain belt in eastern Greenland formed by Paleozoic continental collisions that were part of the broader Caledonian orogenic system spanning present-day North America and Europe.
• B. Sveconorwegian orogeny
  The Sveconorwegian orogeny was a major Mesoproterozoic mountain-building event that shaped much of southwestern Scandinavia, forming part of the ancient basement rocks of the Fennoscandian region.
• 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. Svecofennian orogeny
  The Svecofennian orogeny was a major Paleoproterozoic mountain-building event that formed much of the continental crust of present-day Sweden and Finland within the Fennoscandian Shield.
• E. Karelian orogeny
  The Karelian orogeny was an ancient Paleoproterozoic mountain-building event that shaped much of the bedrock and geological structure of the Fennoscandian Shield in northern Europe.
• F. None of above. chosen