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近年来在我国获得大量的地质、地球物理和地球化学等资料的基础上,特别是将地表地质构造的研究与深部地质构造和新构造运动的研究结合起来,更加深和丰富了对大地构造的认识。 1957年,地质部航测大队首次在我国东部发现了郯城—庐江深大断裂带。同时,大量的地球物理工作,为我国早期油田的勘探与开发提供了地质构造的依据。六十至七十年代,利用人工地震研究地壳和上地幔的结构,提出了部分地区的详细地壳模型和地壳厚度。在我国某些地区开始了古地磁学的研究。七十年代利用大地电磁测深研究
In recent years, based on the large amount of data of geology, geophysics and geochemistry obtained in our country, especially combining the research of surface geological structure with the research of deep geological structure and neotectonic movement, it deepens and enriches the study on the geotectonic understanding. In 1957, for the first time, the navigation team of the geological department discovered the Yuncheng-Lujiang deep fault zone in the eastern part of China. At the same time, a large amount of geophysical work has provided the basis for the geological structure for the exploration and development of the early oilfield in our country. From the 1960s to the 1970s, the earth crust and upper mantle structure were studied using artificial earthquakes, and detailed crustal models and crustal thicknesses in some areas were proposed. In some parts of our country, the study of paleomagnetism began. Seventies using the study of the earth electromagnetic sounding