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济阳坳陷中-新生代断裂发育特征及形成机制

张鹏  王良书  丁增勇  钟锴 

摘 要:济阳坳陷中生代以NW向断裂活动为主;新生代早期盆地发育受NW向和NE向断裂共同控制,沙河街组四段沉积后,以NE向断裂活动为主.济阳坳陷中-新生代断裂活动主要受太平洋板块向欧亚板块的斜向俯冲造成的弧后伸展作用及郯庐断裂的走滑作用联合控制.早白垩世初,太平洋板块向欧亚大陆的俯冲使郯庐断裂带发生左行走滑平移,在济阳地区形成了一系列NW向正断层.新生代早期,济阳坳陷东部断裂活动受郯庐断裂左旋走滑的控制,而西部受弧后伸展作用影响较大.大约43 Ma后,太平洋板块聚敛方向改变,济阳坳陷断裂活动主要受NW-SE向区域伸展作用控制.
关键词:太平洋板块俯冲;断裂活动性;形成机制;郯庐断裂带;中-新生代;济阳坳陷
分类号:TE111.2 文献标识码:A

文章编号:0253-9985(2006)04-0467-08

Characteristics and formation mechanism of the faults in Mesozoic-Cenozoic in Jiyang Depression

Zhang Peng  Wang Liangshu  Ding Zengyong  Zhong Kai 

 

张鹏(1981-),男,博士研究生,盆地构造与地球动力学
作者单位:张鹏(南京大学,地球科学系,江苏,南京,210093) 
     王良书(南京大学,地球科学系,江苏,南京,210093) 
     丁增勇(南京大学,地球科学系,江苏,南京,210093) 
     钟锴(南京大学,地球科学系,江苏,南京,210093) 

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