郯庐断裂带渤海段深、浅构造特征探讨

摘要

In conclusion, the Mesozoic and Cenozoic Bohai segment of the Tan-Lu fault zone have obvious different internalstructures and fault systems, spread ranges and the location of activities. Although this deep and shallow fault systemcan not completely represent all the deep and shallow structural features of the Bohai section, it also can provide a new way to study the characteristics of different segments and resolve the differences and provide a new way to study theevolution of the Bohai Bay basin.