Appalachian–Ouachita–Marathon orogenic system

Target entity: Appalachian–Ouachita–Marathon orogenic system
Context triple: [Ouachita orogeny, overlapsWith, Appalachian–Ouachita–Marathon orogenic system]

• A. Ouachita orogeny
  The Ouachita orogeny was a major Paleozoic mountain-building event that formed the Ouachita Mountains of Arkansas, Oklahoma, and adjacent regions through the collision of ancient continental plates.
• B. Appalachian orogeny
  The Appalachian orogeny was a series of ancient mountain-building events that formed the Appalachian Mountains through the collision of tectonic plates during the Paleozoic Era.
• C. Taconic orogeny
  The Taconic orogeny was an early Paleozoic mountain-building event along the eastern margin of ancient North America that contributed significantly to the formation of the Appalachian Mountains.
• D. Acadian orogeny
  The Acadian orogeny was a major Middle Paleozoic mountain-building event that significantly shaped the northern Appalachian Mountains through the collision of ancient landmasses.
• E. 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.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Target entity: Appalachian–Ouachita–Marathon orogenic system
Target entity description: The Appalachian–Ouachita–Marathon orogenic system is a vast Paleozoic mountain-building belt that once stretched from present-day Canada through the eastern and southern United States into Mexico, formed during the assembly of the supercontinent Pangaea.

• A. Ouachita orogeny
  The Ouachita orogeny was a major Paleozoic mountain-building event that formed the Ouachita Mountains of Arkansas, Oklahoma, and adjacent regions through the collision of ancient continental plates.
• B. Appalachian orogeny
  The Appalachian orogeny was a series of ancient mountain-building events that formed the Appalachian Mountains through the collision of tectonic plates during the Paleozoic Era.
• C. Taconic orogeny
  The Taconic orogeny was an early Paleozoic mountain-building event along the eastern margin of ancient North America that contributed significantly to the formation of the Appalachian Mountains.
• D. Acadian orogeny
  The Acadian orogeny was a major Middle Paleozoic mountain-building event that significantly shaped the northern Appalachian Mountains through the collision of ancient landmasses.
• E. 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.
• F. None of above. chosen