permo-carboniferous was the main period ih the late evolution of craton basin fortarim plate. its prototype basin was formed in the setting of plate convergence.
塔里木板块在石炭-二叠纪是克拉通盆地演化后期的主要阶段,其原型盆地形成于板块会聚背景。
the ordos basin has been being thought as a stable craton basin for a long time by many chinese researchers, in which none of the faults were developed yet.