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| Figure 3: Northern fragment of Ural-African intensive riftogenesis belt.1–4–Stabilized crustal blocks (cover and platform basement): 1-cover of ancient platforms (PZ, MZ); 2-cover of recent platforms (PZ-MZ); 3-Pre-Cambrian fold regions; 4-Phanerozoic fold regions; 5–6-Mobile regions: 5-basement of Mediterranean orogenic belt; 6-eastern terminus of Dniepr-Donets rift; 7–10-zones and regions of intensive continental riftogenesis: 7-linear suture zones with intensive sedimentation (а), mantle magmatism (b) and subsequent folding (Ural-Novaya Zemlya fold system); 8-foredeeps with intensive extension and downwarping; 9-linear riftogenesis (rift) zones; 10-faults: а-proven, b-assumed; 11-regions of polygonal riftogenesis; 12-thickness of sedimentary deposits; 13-oil (а) and gas (b) fields; 14-approximate boundary of Ural-African intercontinental belt. |
