ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
再论奥陶系与志留系界线的划分与对比
  
关键词:
基金项目:
作者单位
汪啸风 中国地质科学院宜昌地质矿产研究所 
曾庆銮 中国地质科学院宜昌地质矿产研究所 
周天梅 中国地质科学院宜昌地质矿产研究所 
倪世钊 中国地质科学院宜昌地质矿产研究所 
项礼文 中国地质科学院地质研究所 
赖才根 中国地质科学院地质研究所 
摘要点击次数: 4922
全文下载次数: 6004
摘要:
REDISCUSSION ON THE DIVISION AND CORRELATION OF THE ORDOVICIAN-SILURIAN BOUNDARY
      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).
WANG Xiao-feng,ZENG Qing-luan,ZHOU Tian-mei,NI Shi-zhao,XIANG Li-wen,LAI Cai-gen.1986.REDISCUSSION ON THE DIVISION AND CORRELATION OF THE ORDOVICIAN-SILURIAN BOUNDARY[J].Acta Geoscientica Sinica,8(1):157-175.
查看全文  查看/发表评论  下载PDF阅读器
Copyright©2008 All Rights Reserved
Sponsored by:
Address:: PostCode: Tel: E-mail: