Contrasts in the Quaternary of mid-North
β
H. E. Wright
π
Article
π
2005
π
John Wiley and Sons
π
English
β 688 KB
## Abstract The West Siberian Plain was formed by marine deposits that extended from the Mediterranean basin to the arctic. Tectonic action later produced a striking series of long straight NEβSW grabens in the southern part of the plain. Pleistocene advance of the Kara ice sheet onto the continent