TY  JOUR
TI  Geological complexes in the margin of the Siberian Craton as indicators of the evolution of a Neoproterozoic Supercontinent
KW  Siberian Craton
KW  evolution of a Neoproterozoic Supercontinent
KW  Late Precambrian geologic complexes.
JO  Russian Journal of Earth Sciences
AU  Sklyarov, E.V.
AU  Gladkochub, D.P.
AU  Mazukabzov, A.M.
AU  Donskaya, T.V.
AU  Stanevich, A.M.
PY  2002
IS  4
PB  Geophysical Center of the Russian Academy of Sciences