1958  Chang, p.85: Classic sediments in Suhuho area and
           represented by conglomerates, sandstones, shales and
           limestones; but the type Clymeneenkalk predominating
           near Taminshan area represented by pinkish limestones.
     1960  Chang, p.189: 1.45 km E of the NE crest, near
           Taminshan, Pie-cu, Mei-tou-ho, Great Khingan, Inner
           Mongolia.