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Clastic dikes of Volga region

Distanov, U.G.

Arenaceous branching dikes in sedimentary formations range in thickness from several centimeters to 2 m; most of these dikes are believed to be result of squeezing caused by underwater landslides. (See also Akademiya Nauk SSSR, Doklady v 160 n 5 1965 p 1159-61)

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Clastic dikes of Volga region

Distanov, U.G.

Arenaceous branching dikes in sedimentary formations range in thickness from several centimeters to 2 m; most of these dikes are believed to be result of squeezing caused by underwater landslides. (See also Akademiya Nauk SSSR, Doklady v 160 n 5 1965 p 1159-61)

Clastic dikes of Volga region

Distanov, U.G.

Arenaceous branching dikes in sedimentary formations range in thickness from several centimeters to 2 m; most of these dikes are believed to be result of squeezing caused by underwater landslides. (See also Akademiya Nauk SSSR, Doklady v 160 n 5 1965 p 1159-61)

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Title:

Clastic dikes of Volga region

Additional title:

O klasticheskikh daikakh Povolzh'ya

Contributors:

Distanov, U.G. (author)

Published in:

Doklady of the Academy of Sciences of the USSR -- Earth Science Section ; 160

Publication date:

1965

Size:

3 pages

Type of media:

Article (Journal)

Type of material:

Print

Language:

English

Keywords:

© Metadata Copyright Elsevier B. V. All rights reserved.

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