THE PLIOCENE LACUSTRINE SERIES IN CENTRAL SHANSI
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    摘要:

    Ⅰ.HISTORICAL CONSPECTUS For years,the Pliocene deposits of North China,have been chieflyknown by the "slopes-facies" of their lowest horizons (Hipparion richtho-feni Pontian red clays,see:Andersson 1923).Gradually however,the pre-sence of extensive freshwater formations belonging to this age,has become

    Abstract:

    Ⅰ.HISTORICAL CONSPECTUS For years,the Pliocene deposits of North China,have been chieflyknown by the "slopes-facies" of their lowest horizons (Hipparion richtho-feni Pontian red clays,see:Andersson 1923).Gradually however,the pre-sence of extensive freshwater formations belonging to this age,has become

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E. LICENT, M. TRASSAERT.1935. THE PLIOCENE LACUSTRINE SERIES IN CENTRAL SHANSI[J].地质学报,(2).
E. LICENT, M. TRASSAERT.1935.[J]. Acta Geologica Sinica,(2).

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