the Thermal stream and an arrangement of ruptures. An average europas

you are: the Thermal stream and an arrangement of ruptures

Average Europe. Ruptures of northwest and northeast prodeleting Here prevail. Meridionalnoe the direction also is shown often whereas shirotnye structures are found out only at indirect (geophysical) measurements. Infringements of northwest prodeleting are especially characteristic for southwest restriction of the East European platform; dogertsinskie on age, they supervised orientation of pools osadkonakoplenija (molassovyh hollows) postorogenicheskoj development stages gertsinskogo, or varisskogo, a folded belt and were the main system during all mezozoja and kajnozoja (the basic activity between doggerom and paleotsenom); prevailed vertical and nadvigovye movements. The system of northeast prodeleting also has arisen in dogertsinskoe time. It supervised development of pools osadkonakoplenija along southern edge of the Central European hollow. In tertiary time (paleotsen - miotsen) movements on this system have renewed in all territory of Average Europe and had mainly character of a stretching.