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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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Titel:

Clastic dikes of Volga region

Weitere Titelangaben:

O klasticheskikh daikakh Povolzh'ya

Beteiligte:

Distanov, U.G. (Autor:in)

Erschienen in:

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

Erscheinungsdatum:

1965

Format / Umfang:

3 pages

Medientyp:

Aufsatz (Zeitschrift)

Format:

Print

Sprache:

Englisch

Schlagwörter:

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

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