The longest one in Asia is called the Altyn Tagh. These structures commonly end with radiating normal structures called horsetail splays.  Enechelon folds commonly occur on either side of them, and mountain ranges may form when one encounters a restraining bend.  Indent-linked ones like the Red River carry material away from transpression zones, and transform ones connect convergent and divergent plate boundaries.  Classified as "sinistral" or "dextral," FTP, name this type of fault characterized by horizontal displacem
The longest one in Asia is called the Altyn Tagh. These structures commonly end with radiating normal structures called horsetail splays.  Enechelon folds commonly occur on either side of them, and mountain ranges may form when one encounters a restraining bend.  Indent-linked ones like the Red River carry material away from transpression zones, and transform ones connect convergent and divergent plate boundaries.  Classified as "sinistral" or "dextral," FTP, name this type of fault characterized by horizontal displacement along the fracture plane, whose best known example is the San Andreas.
The longest one in Asia is called the Altyn Tagh. These structures commonly end with radiating normal structures called horsetail splays.  
strike-slip fault (PROMPT on just "fault.")