Issue 49

A. Akhmetov et alii, Frattura ed Integrità Strutturale, 49 (2019) 190-200; DOI: 10.3221/IGF-ESIS.49.20

Figure 2: Orientation of the (1) Batolit-1982 and (2) Shpat geological profiles crossing the Yenisei Ridge.

(а)

(b) Figure 3: Structural models of deep layers of the Yenisei Ridge along the (а) Batolit-1982 and (b) Shpat profiles.

These profiles reveal crustal layers and a 10–12 km deep lens in the Yenisei Ridge with different geological, physical and mechanical properties.

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