Qinling–Dabie orogeny

Target entity: Qinling–Dabie orogeny
Context triple: [Dabie Mountains, orogeny, Qinling–Dabie orogeny]

• A. Yanshanian orogeny
  The Yanshanian orogeny was a major Mesozoic mountain-building event in northern China that significantly reshaped the geology and structure of the Yan Mountains and surrounding regions.
• 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. Karakoram orogeny
  The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Target entity: Qinling–Dabie orogeny
Target entity description: The Qinling–Dabie orogeny was a major Paleozoic–Mesozoic mountain-building event in central China that formed the Qinling and Dabie mountain ranges through the collision of the North China and South China tectonic blocks.

• A. Yanshanian orogeny
  The Yanshanian orogeny was a major Mesozoic mountain-building event in northern China that significantly reshaped the geology and structure of the Yan Mountains and surrounding regions.
• 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. Karakoram orogeny
  The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
• F. None of above. chosen