THE JINNING MOVEMENT IN THE DONGZHI AREA OF SOUTH ANHUI
SUN Cheng - yun, CHU Jin - hai, GENG Xiao - guang, WU Jia - fu, XIE Jian - cheng (Anhui Academy of Geological Survey, Hefei 230001, China )
The Jinning Movement in the Dongzhi area of South Anhui is expressed as a substantially EW - trending linear tight isoclinal overturn fold in its early period, NW - to SN - trending isoclinal overturn fold in its late period and NE - to NEE - trending open fold with occurrence of complicated superposition of folds in the end. The field evidences indicate the presense of two significant dis continuities that delimited three tectonic strata of the mid - late Proterozoic era.
【CateGory Index】： P542