中國有色金屬學(xué)報(英文版)
Transactions of Nonferrous Metals Society of China
| Vol. 8 No. 1 March 1998 |
GEOLOGICAL FEATURE OF YUNKAI RIFT
Li Peizheng, Zeng Xiaodong and Deng Jiqiu
（College of Resource, Environment and Civil Engineering,Central South University of Technology, Changsha 410083, P. R. China）
Abstract:The Yunkai area, which spreads along the boundary between Guangdong and Guangxi, is a terrain with independent structure unit and evolution history. The features of the rigid basement, egde faults, sedimentary formation, alkalic basic volcanism, metamorphic facies series and geophysical anomalies of this area indicate that the Yunkai terrain was formed in the geosynclinal-type rift caused by the rigid crust extension at Sinian period of upper Proterozoic subera.
Key words: Yunkai rift edge faults sedimentary formation evolution histor
