Mit 7 Abbildungen und 1 Tabelle
ZusammenfassungErgebnisse seismiseher Untersuchungen der Erdkruste sowie andcrer geophysikalischer und derzeitiger geologiseher Daten gestatteten es den Autoren, die seismisehen Auflagergrenzen geologiseh zu interpretieren. Auf diese Grenzen bezogene Strukturschemata, die Fahenkomplexe versehiedenen Alters in der Erdkruste voneinander trennen, werden konstruiert. Es stellt sieh die geologische Natur einer ,,Basaltschieht" heraus. Es zeiehnet sieh die zeitliche Aufeinanderfolge der Evolution der Erdkruste ab.
AbstractDeep formations of the Caucasus and surrounding area are presented on the basis of seismic and geological data. Thickness of seismic sections and its geological age are considered. The geological nature of a "basalt" layer of the earth's crust is discussed. Successive changes in the earth's crust in the process of evolution of geosynclinal depression are presented.
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