Basin and Range extensional tectonic regime

Target entity: Basin and Range extensional tectonic regime
Context triple: [Willcox Basin, geologicalSetting, Basin and Range extensional tectonic regime]

• A. Basin and Range–Salton Trough transition zone
  The Basin and Range–Salton Trough transition zone is a tectonically active region in southern California where the extensional Basin and Range Province meets the pull-apart Salton Trough along the plate boundary between the Pacific and North American plates.
• B. Basin and Range–Colorado Plateau transition
  The Basin and Range–Colorado Plateau transition is a geologic boundary zone in the southwestern United States where the highly extended Basin and Range Province meets the relatively stable, uplifted Colorado Plateau, producing complex faulting, volcanism, and varied topography.
• C. Wyoming Basin and Range transition
  The Wyoming Basin and Range transition is a geologic province in western Wyoming marking the structural and topographic boundary between the high, rugged ranges of the Rocky Mountains and the more subdued basins and ranges to the west and south.
• D. Continental Borderland basins
  Continental Borderland basins are a series of deep, fault-controlled submarine depressions off the coast of Southern California that record complex tectonic and sedimentary processes along the Pacific–North America plate boundary.
• E. Pacific coastal plain from interior desert basins
  The Pacific coastal plain from interior desert basins is a low-lying, ocean-adjacent region along the Baja California Peninsula characterized by relatively flat terrain and a more moderate, maritime-influenced climate compared with the arid interior deserts.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Target entity: Basin and Range extensional tectonic regime
Target entity description: The Basin and Range extensional tectonic regime is a broad region of the western United States characterized by crustal stretching that produces alternating mountain ranges and sediment-filled basins.

• A. Basin and Range–Salton Trough transition zone
  The Basin and Range–Salton Trough transition zone is a tectonically active region in southern California where the extensional Basin and Range Province meets the pull-apart Salton Trough along the plate boundary between the Pacific and North American plates.
• B. Basin and Range–Colorado Plateau transition
  The Basin and Range–Colorado Plateau transition is a geologic boundary zone in the southwestern United States where the highly extended Basin and Range Province meets the relatively stable, uplifted Colorado Plateau, producing complex faulting, volcanism, and varied topography.
• C. Wyoming Basin and Range transition
  The Wyoming Basin and Range transition is a geologic province in western Wyoming marking the structural and topographic boundary between the high, rugged ranges of the Rocky Mountains and the more subdued basins and ranges to the west and south.
• D. Continental Borderland basins
  Continental Borderland basins are a series of deep, fault-controlled submarine depressions off the coast of Southern California that record complex tectonic and sedimentary processes along the Pacific–North America plate boundary.
• E. Pacific coastal plain from interior desert basins
  The Pacific coastal plain from interior desert basins is a low-lying, ocean-adjacent region along the Baja California Peninsula characterized by relatively flat terrain and a more moderate, maritime-influenced climate compared with the arid interior deserts.
• F. None of above. chosen