同生断裂的幕式活动，引起沉积环境的改变，形成了毒重石和重晶石的互层。
Moreover, episodic activities of the growth faults changed the sedimentary environment and resulted in the interbedding of witherite and barite ores.
同生断裂的幕式活动，引起沉积环境的改变，形成了毒重石和重晶石的互层。
Moreover, episodic activities of the growth faults changed the sedimentary environment and resulted in the interbedding of witherite and barite ores.
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