fig06.htm

Figure 6. (a) Vertical section of the tectonic breaking (1-1') plotted along the Azau-Baksan Profile. (1) Lithosphere tectonic breaking contour lines: thick lines are multiples of 10 arbitrary units, thin lines show intermediate values; (2, 3) results of interpreting the data recorded using the method of earthquake reflected waves (after S. A. Agamirzoev): (2) nearly horizontal boundaries inside the crust, (3) inclined fault zones; (4) observation site; (b) vertical (submeridional) section across the field of the tectonic breaking of the lithosphere (2-2') plotted across the Caucasus strike and passing across the Elbrus peak; (5) inferred crustal interfaces; (c) vertical section of tectonic breaking (3-3') plotted along the Caucasus strike and passing through the Elbrus peak (nearly latitudinal): (1) contour lines of the tectonic breaking of the lithosphere: thick lines show the values, multiple of 10 arbitrary units, thin lines show intermediate values; (6) nearly horizontal boundaries in the crust, identified on the basis of a specific tectonic disintegration pattern; (7, 8) regions of abnormally low values of the tectonic breaking field: (7) highly anomalous, (8) moderately anomalous.


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