The Influence of an Interdependent Structures on the Post-Mesozoic Evolution of the Eastern Flank of the Mongol-Okhotsk Orogenic Belt

Based on the analysis of known geodynamic models that explain processes in various settings Meso-Cenozoic stages development continental margins and tectonic-magmatic events accompanying these processes, as well basis our own data obtained a result many years research axial structure Central Asian Fold Belt-Mongol-Okhotsk orogenic belt influence interdependent structures post-Mesozoic evolution eastern flank Mongol-Okhotsk was substantiated by us. The closure basin due to approach Siberian North China cratons accompanied change conditions: subduction, collision, intraplate-rift reflected formation synchronous igneous complexes frame belt. In northern belt, distribution magmatites is cut off Selenga-Stanovoy superterrane west. boundary zone Dzheltulak fault. south, it borders along tectonic melange. We believe evolutionary within its framing continued into time after final an orogen. position late Mesozoic did not correspond modern one. fold located between craton Cenozoic were influenced collisional occurring Indian Eurasian plates. And only “driving force” for movement time, but also changed orogen, dividing two flanks.