Up to 1931 nothing was positively known concerning the Cenozoicformations eventually preserved in S.E.Shansi.The large area bounded by
P. TEILHARD DE CHARDIN, C. C. YOUNG.1933.[J].地质学报,(0).
P. TEILHARD DE CHARDIN, C. C YOUNG.1933. THE LATE CENOZOIC FORMATIONS OF S. E. SHANSI[J]. Acta Geologica Sinica,(0).
