ON THE CAMBRIAN AND THE ORDOVICIAN FORMATIONS OF HSISHAN OR WESTERN HILLS OF PEKING
DOI:
Author:
Affiliation:
Clc Number:
Fund Project:
Article
|
Figures
|
Metrics
|
Reference
|
Related
|
Cited by
|
Materials
|
Comments
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
Reference
Related
Cited by
Get Citation
.1927. ON THE CAMBRIAN AND THE ORDOVICIAN FORMATIONS OF HSISHAN OR WESTERN HILLS OF PEKING[J]. Acta Geologica Sinica(),6(2):
