Weibei basin is a Mesozoic-Cenozoic basin developed in the Tanlu fault zone.
潍北盆地是发育于郯庐断裂带内的中、新生代盆地。
Abundant pyroxenite xenoliths were found from the Cenozoic Changle basalts, an area distributing near the Tanlu fault zone.
紧邻郯庐断裂带分布的山东昌乐新生代玄武岩含有丰富的辉石岩捕虏体。
In the Triassic period, following the collision between North-China and South-China cratons, the Tanlu fault zone was formed.
三叠纪，华南与华北克拉通碰撞，郯庐断裂带形成。
The Tanlu fault zone, a NNE fault zone in east China, has a complex internal structure and a broad scale. It is about 2400km long within China.
郯庐断裂带是中国东部一条结构复杂、规模巨大的北北东向断裂构造带，在我国境内长达2400多公里。
Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu (TanchengLujiang) fault zone.
合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。
Tanlu strike-slip fault zone had experienced several phases of movement, exerting strong influence and control upon the hydrocarbon pooling within the zone.
郯庐走滑断裂带经历了多期活动，影响和控制走滑断裂带内的油气成藏。
Tanlu strike-slip fault zone had experienced several phases of movement, exerting strong influence and control upon the hydrocarbon pooling within the zone.
郯庐走滑断裂带经历了多期活动，影响和控制走滑断裂带内的油气成藏。
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