The late Pli cene freshwater Taiku Deposits developed in tnebasin behind the great Taiku fault-scarp in central Shansi,have alreadybeen thoroughly described stratigraphically as well as technically by Dr.Barbour~1 and later by P.Teilhard and Dr. Young~2.However,it seems
Abstract:
The late Pli cene freshwater Taiku Deposits developed in tnebasin behind the great Taiku fault-scarp in central Shansi,have alreadybeen thoroughly described stratigraphically as well as technically by Dr.Barbour~1 and later by P.Teilhard and Dr. Young~2.However,it seems
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陈国达.1936. A NOTE ON THE SUBAQUATIC DEFORMATION IN THE TAIKU DEPOSITS[J]. ACTA GEOLOGICA SINICA(English edition),15(4):
