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《Journal of Stratigraphy》 1983-03
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Problems of Eumorphotes-bearing strata of the"Shihchienfeng Formation" in Qish-an, Shaanxi

Cheng Zheng-wit, Qu Li-fan, Hou Jing-peng and Li Pei-xian  
The "Liujiagou Formation", being in fault-contact with the underlying Shihchienfeng Formation, is lithologically identical to the " Shihchienfeng Formation" in Houzhougong-miao and contains also the Lundbladispora-Taeniaesportes-Cycadopites assemblage and marine bivalve Pteria cf. murchisoni of Early Triassic Olenekian age. Hence the Eumorphotis-bearing "Shihehienfeng Formation" is not equivalent to the true Shihchienfeng Formation; it should rather belong to the "Liujiagou Formation" in Zishiya except that it represents a facies (littoral to nexitie) different from that represented by the latter. Here the name, the Qishan Formation proposed by the Third Exploration Brigade (1975) was used. The two bivalve horizons mentioned above show that the Liujiagou Formation is largely equivalent to the Induan-Lower Olenekian. This supports the conclusion drawn from the study of terrestrial fossils in North China, i. e. the Shihchienfeng Formation belongs to the Upper Permian, while the Liujiagou and Heshanggou Formations to the Lower Triassic.
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