“…Burlin & Stoupakova (2008). Modified from Bogdanov & Khain (1996a, b), Milanovskiy (1987Milanovskiy ( , 1991, Gabrielsen et al (1990), Johansen (1994), Suprunenko et al (2004) and Filatova & Khain (2007). 1, Stable platform areas; 2, intracratonic rift systems with inherited extensional depressions and inverted swells; 3, inverted swells; 4, sag basins, overlying older structures; 5, domes and uplifts; 6, Baikalian folding; 7, Caledonian folding; 8, Hercynian folding; 9, Cimmerian folding: a, more dislocated; b, less dislocated; b, poorly dislocated; 10, volcanic belts; 11, oceanic rifting; 12, deep faults; 13, continental slope margin; 14, coast line.…”