尽管世界上许多科学家做了很大努力,但有关南极地壳构造的地球物理研究仍处于踏勘阶段。迄今,航空地球物理测量仅集中在有限规模的几个地区,而且尚未采用有效的综合方法。最近利用射电回声探测对南极广大内陆区进行了测量,这对于了解南极冰川下的构造有非常重要的贡献。然而,这种测量,几乎没有任何地方兼有深部地壳研究。因此,基岩起伏特征与地壳构造的关系,在更大程度上,仍然依据全球的类比,而较少依据直接获得的南极 Despite the great efforts of many scientists in the world, the geophysical research on the Antarctic crustal structure is still under exploration. To date, aerospace geophysical surveys have focused on only a limited number of areas and have not yet adopted an effective integrated approach. The recent survey of the vast Antarctic interior region using radio echo measurements has made a significant contribution to the understanding of the structure beneath the Antarctic glacier. However, there are few studies of deep crust in this kind of survey. Therefore, the relationship between the bedrock undulations and the crustal structure is still to a large extent based on global analogies, and less on the basis of direct access to Antarctica