赣榆—焦作由东向西深部挤压带

赣榆－焦作由东向西深部挤带是作用提出的新观点，深部挤压发生在上地幔和下地壳，由黄海下部上地幔的扩攻作用产生，从大量的地球物理、浅层构造、应力和应变资源反映它的存在，该带控制了大量强烈的地震的发生，预测将来会有强烈地震发生在挤压带的北侧，推测挤压带深部有大量的地热资源。

The Westward Deep Thrust Zone across Ganyu and Jiaozou

The existance of a westward deep thrust zone is for the first time advanced by the author. The deep thrust which acted mainly on the upper mantle and lower crust and strongly affected the superstructures was formed by the westward spreading of the upper mantle under the Yellow Sea. The deep thrust zone and its characteristics were disclosed on the basis of a variety of geophysical data, surface tectonic features, and the data of stress and strain. Many strong earthquakes distributed on the northern side of the zone were controlled by the deep thrust. It is predicted that the strong earthquakes will occur on the northern side of the zone in future,and that there exist rich geothermal resources along the zone.