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本文的目的是根据地震测深结果综述有关地中海造山区岩石圈结构的资料。在此基础上,将注意到两个方面的问题:在壳—幔界面有明显位移的地壳结构所具有的横向不均匀性以及这种特点的构造意义。图1是以往在地中海地区用折射波方法所作的地震测线图(到1981年以前的工作)。图2则表明本文所讨论的地震剖面的测线位置。
The purpose of this paper is to summarize information on lithospheric structures in the orogenic regions of the Mediterranean, based on the results of seismic sounding. On this basis, two problems will be noticed: the lateral inhomogeneity of the crustal structure with obvious displacement at the crust-mantle interface and the structural significance of this feature. Figure 1 shows the seismograms previously used in the Mediterranean region by the refraction method (until 1981). Figure 2 shows the line location of the seismic section discussed in this article.