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Tanlu

Tanlu

Tanlu

Tanlu

1

The Tanlu ductile brittle shear zone is the major structure as passageway for ore fluid and its secondary faults are the main host.

郯庐韧 —脆性剪切带是主要的导矿构造，其次级断裂是主要容矿场所。

2

Subei-south Huanghai Basin and Bohai Bay Basin are distributed symmetrically on the side of Tanlu fault , and are separated by Lusu uplift .

苏北 -南黄海盆地与渤海湾盆地之间以鲁苏隆起相隔，对称分布于郯庐断裂两侧。

3

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。

4

5

second, secondary migration through the discordogenic fault related to Tanlu fault ;

二是通过与郯庐断裂有关的深大断裂二次运移；

6

Tanlu fracture belt ;

郯庐系断裂带；

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