Jiaolai basin is a strike-slip and pull-apart basin controlled by the Yishu Fault Belt and Wulian -jimo-muping Fault.
胶莱盆地是中生代走滑拉分盆地，其形成与发育受到沂沭断裂和五莲-即墨-牟平断裂的控制。
The Jiaolai strike-slip pull-apart basin is characterized by: 1 shallow-water sequences along the strike-slip faults and deep-water sequences far from the strike-slip faults;
胶莱走滑拉分盆地层序特征表现为：（1）靠近走滑断层的区域发育浅水型层序，而远离走滑断层的区域发育深水型层序；
The Jiaolai strike-slip pull-apart basin is characterized by: 1 shallow-water sequences along the strike-slip faults and deep-water sequences far from the strike-slip faults;
胶莱走滑拉分盆地层序特征表现为：（1）靠近走滑断层的区域发育浅水型层序，而远离走滑断层的区域发育深水型层序；
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