Cambro-Ordovician rocks occur widely in Hsishan. In the westernenvirons of Peking some of the best exposures of these rocks can be observedin the Northern limb of the Chiulungshan (九山龙) syncline, which extends
Abstract:
Cambro-Ordovician rocks occur widely in Hsishan. In the westernenvirons of Peking some of the best exposures of these rocks can be observedin the Northern limb of the Chiulungshan (九山龙) syncline, which extends
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黄汲清.1927. ON THE CAMBRIAN AND THE ORDOVICIAN FORMATIONS OF HSISHAN OR WESTERN HILLS OF PEKING[J]. ACTA GEOLOGICA SINICA(English edition),6(2):
