Late Riphean alkaline magmatism in the western margin of the Siberian Craton: A result of continental rifting or accretionary events?

Doklady Earth Sciences

Volumn 419, Issue 1, 2008, Pages 226-230

  Vernikovsky, V A ^a   Vernikovskaya, A E ^a   Sal'nikova, E B ^b   Berezhnaya, N G ^c   Larionov, A N ^c   Kotov, A B ^b   Kovach, V P ^b   Vernikovskaya, I V ^a   Matushkin, N Yu ^a   Yasenev, A M ^a  

^a TROFIMUK INSTITUTE OF PETROLEUM GEOLOGY AND GEOPHYSICS   (Russian Federation)

^b INSTITUTE OF PRECAMBRIAN GEOLOGY AND GEOCHRONOLOGY   (Russian Federation)

^c A P KARPINSKY RUSSIAN GEOLOGICAL RESEARCH INSTITUTE   (Russian Federation)

Author keywords

[No Author keywords available]

Indexed keywords

ACCRETION; ALKALINE ROCK; MAGMATISM; RIFTING; RIPHEAN; TECTONIC EVOLUTION;

EURASIA; RUSSIAN FEDERATION; SIBERIAN CRATON;

EID: 55949135800     PISSN: 1028334X     EISSN: None     Source Type: Journal    
DOI: 10.1134/S1028334X08020086     Document Type: Article

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