Wilson cycle of Pangaea assembly

Target entity: Wilson cycle of Pangaea assembly
Context triple: [Rheic Ocean, partOf, Wilson cycle of Pangaea assembly]

• A. Neoproterozoic supercontinent cycle
  The Neoproterozoic supercontinent cycle refers to the sequence of assembly and breakup of supercontinents during the Neoproterozoic Era, including the formation and fragmentation of Rodinia and the tectonic, climatic, and biological changes associated with these events.
• B. Gondwana amalgamation
  Gondwana amalgamation refers to the late Neoproterozoic–early Paleozoic tectonic assembly of the supercontinent Gondwana through the collision and suturing of multiple continental blocks and terranes.
• C. supercontinent Pangaea
  Pangaea was a massive supercontinent that existed during the late Paleozoic and early Mesozoic eras, when nearly all of Earth's landmasses were joined together before breaking apart into the continents we know today.
• D. supercontinent Rodinia
  Rodinia was an ancient supercontinent that assembled during the Proterozoic Eon and existed before the later supercontinent Pangaea, profoundly influencing Earth’s early tectonic and climatic evolution.
• E. Precambrian Shield formation
  The Precambrian Shield formation is an ancient, stable core of the Earth's crust composed mainly of very old igneous and metamorphic rocks that underlies much of central and eastern Canada and parts of the northern United States.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Target entity: Wilson cycle of Pangaea assembly
Target entity description: The Wilson cycle of Pangaea assembly refers to the full tectonic life cycle in which ancient oceans opened and later closed through plate convergence, culminating in the formation of the supercontinent Pangaea.

• A. Neoproterozoic supercontinent cycle
  The Neoproterozoic supercontinent cycle refers to the sequence of assembly and breakup of supercontinents during the Neoproterozoic Era, including the formation and fragmentation of Rodinia and the tectonic, climatic, and biological changes associated with these events.
• B. Gondwana amalgamation
  Gondwana amalgamation refers to the late Neoproterozoic–early Paleozoic tectonic assembly of the supercontinent Gondwana through the collision and suturing of multiple continental blocks and terranes.
• C. supercontinent Pangaea
  Pangaea was a massive supercontinent that existed during the late Paleozoic and early Mesozoic eras, when nearly all of Earth's landmasses were joined together before breaking apart into the continents we know today.
• D. supercontinent Rodinia
  Rodinia was an ancient supercontinent that assembled during the Proterozoic Eon and existed before the later supercontinent Pangaea, profoundly influencing Earth’s early tectonic and climatic evolution.
• E. Precambrian Shield formation
  The Precambrian Shield formation is an ancient, stable core of the Earth's crust composed mainly of very old igneous and metamorphic rocks that underlies much of central and eastern Canada and parts of the northern United States.
• F. None of above. chosen