%0 Journal Article
%T REDISCUSSION ON THE DIVISION AND CORRELATION OF THE ORDOVICIAN-SILURIAN BOUNDARY<br>再论奥陶系与志留系界线的划分与对比
%A WANG Xiao-feng
%A ZENG Qing-luan
%A ZHOU Tian-mei
%A NI Shi-zhao
%A XIANG Li-wen
%A LAI Cai-gen
%A <br>汪啸风
%A 曾庆銮
%A 周天梅
%A 倪世钊
%A 项礼文
%A 赖才根
%J 地球学报
%D 1986
%I 
%X Some of our views on the correlation of graptiolite and some shelly fossil sequence from the latest Ordovician to earlist Silurian and on the division of the Ordovician-Silurian boundary have been presented in the past papers(Wang et al., 1980, 1983a, b; Lai et al., 1982; Xu et al., 1983). The present paper will further inquire into these problems in the light of biostratigraphy, isotope age dating sedimenatry facies and priliminary paleomagnetic research from the Ordovician-Silurian boundary sections of the eastern Yangzi(Yangtze) Gorges(pl.1-2).
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=1DF69A47DE80569EC8F859DF61571180&aid=8A5BBB6F6CE57A260CD937524F1BF11D&yid=4E65715CCF57055A&vid=5D311CA918CA9A03&iid=CA4FD0336C81A37A&sid=0B4F496D54044D86&eid=A58CF3BAE79427D0&journal_id=1006-3021&journal_name=地球学报&referenced_num=0&reference_num=0