About: White Sea Rift System

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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 . 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 f

Attributes	Values
rdf:type	building
rdfs:label	White Sea Rift System (en)
rdfs:comment	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 . 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 f (en)
foaf:depiction
dcterms:subject	Mesoproterozoic Mesoproterozoic rifts and grabens Geology of European Russia
Wikipage page ID	47584929 (xsd:integer)
Wikipage revision ID	1073461461 (xsd:integer)
Link from a Wikipage to another Wikipage	Mesoproterozoic Proterozoic Barents Sea Jotnian Riphean (stage) East European Craton Intrusion Mesoproterozoic rifts and grabens Cenozoic White Sea Geology of European Russia Paleozoic Graben Rift Magmas Rift Supercontinent dbr:Palaeopangea
sameAs	White Sea Rift System White Sea Rift System White Sea Rift System
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thumbnail	wiki-commons:Special:FilePath/Red_pog.svg?width=300
caption	Location of Kerets Graben, one of many grabens in the White Sea. (en)
float	right (en)
relief	1 (xsd:integer)
width	300 (xsd:integer)
has abstract	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 . 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. The White Sea Rift System includes the following rifts: * the Onega–Kandalaksha Rift (its northwestern graben is known as the Kandalaksha Trough or Kandalaksha Graben). 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. (en)
gold:hypernym	Complex
prov:wasDerivedFrom	wikipedia-en:White_Sea_Rift_System?oldid=1073461461&ns=0
page length (characters) of wiki page	3063 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:White_Sea_Rift_System
is rdfs:seeAlso of	Barents Sea Jotnian Geology of Russia White Sea
is Link from a Wikipage to another Wikipage of	Onega Bay Kandalaksha Gulf Kandalaksha Graben Kandalaksha Trough
is Wikipage redirect of	Kandalaksha Graben Kandalaksha Trough
is foaf:primaryTopic of	wikipedia-en:White_Sea_Rift_System

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