White Sea Rift System Explained

The White Sea Rift System is a complex of rifts manifested as numerous individual grabens located chiefly in the White Sea but including onshore areas and a strip of the Barents Sea. The rifts run in a subparallel manner from northwest to southeast where the rift system continues under the East European Platform. The system or complex originated due to extensional tectonics acting during the Middle to Late Riphean in the Proterozoic. This tectonic environment is believed to have been related to the break-up of the ancient supercontinent Palaeopangea. During the Riphean the graben structures were filled by Jotnian sediments. During the Middle Paleozoic the rift system was reactivated resulting in intrusion of alkaline magmas. In the Late Cenozoic the rift system was reactivated again resulting in the formation of the modern White Sea.^[1]

The White Sea Rift System includes the following rifts:^[1]

• the Onega–Kandalaksha Rift (its northwestern graben is known as the Kandalaksha Trough or Kandalaksha Graben).^[2] The Kandalksha graben is about 220 km long and 60 km broad. Its southwestern slopes are steeper than its northwestern slopes.
• the Kerets–Leshukonsky Rift (including the Kerets Graben).
• the Barents Rift.

Many of the grabens are filled with Jotnian sediments.^[1]

Notes and References

1. Baluev . A.S. . 2006 . Geodynamics of the Riphean stage in the evolution of the northern passive margin of the East European Craton . . 40 . 3 . 183–196 . 10.1134/s0016852106030034. 129043120 .
2. Book: Goodwinn . Alan M.. 1991 . Precambrian Geology . Academic Press . 374 . 978-0122898709 .