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地壳主要构造单元和地幔的不均匀性地震学和重力学的最新成果表明,至200—1000公里深度追踪到与新生代褶皱带、洋中脊和克拉通(前寒武地台)这样三种构造有关的不均匀性。新生代褶皱带形成于洋壳俯冲带或大陆地台向褶皱构造下俯冲带附近。在此两种情况
Incompatibilities of major tectonic units and mantle of the crust The latest achievements in seismology and gravimetry show that up to 200-1000 kilometers of depth are traced to three types of sedimentary facies similar to the Cenozoic fold belt, mid-ocean ridge and craton (Pre-Cambrian platform) Structure-related inhomogeneities. The Cenozoic fold belt was formed in the subduction zone of the oceanic crust or the platform fold fold in the mainland. In both cases