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  , ..
AU  , ..
AU  , ..
AU  , ..
AU  , ..
PY  2002
IS  4
PB  Геофизический центр Российской Академии Наук