IVPP-IR
Chinese Continental Paleocene-Eocene Boundary and Its Correlation
WANG Yuanqing; TONG Yongsheng; LI Qian
2011
发表期刊actageologicasinica
ISSN1000-9515
卷号085期号:002页码:443
摘要Recent paleontological, paleomagnetic and carbon isotopic investigations have provided new evidence supporting placement of the Chinese terrestrial Paleocene-Eocene boundary at the base of the Lingcha Formation in the Hengyang Basin, Hunan Province, and within the upper part of the Nomogen Formation in the Erlian Basin, Inner Mongolia. Based on mammalian and ostracod biostratigraphic data, the boundary can also be roughly correlated with the contacts between the Baoyue and Huayong formations in the Sanshui Basin of Guangdong, the Qingjiang and Xinyu formations of Jiangxi, the Fourth Formation of the Funing Group and the Dainan Formation in northern Jiangsu, and the Dabu and Shisanjianfang formations in the Turfan Basin of Xinjiang.
语种英语
文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/11166
专题中国科学院古脊椎动物与古人类研究所
作者单位中国科学院古脊椎动物与古人类研究所
第一作者单位中国科学院古脊椎动物与古人类研究所
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WANG Yuanqing,TONG Yongsheng,LI Qian. Chinese Continental Paleocene-Eocene Boundary and Its Correlation[J]. actageologicasinica,2011,085(002):443.
APA WANG Yuanqing,TONG Yongsheng,&LI Qian.(2011).Chinese Continental Paleocene-Eocene Boundary and Its Correlation.actageologicasinica,085(002),443.
MLA WANG Yuanqing,et al."Chinese Continental Paleocene-Eocene Boundary and Its Correlation".actageologicasinica 085.002(2011):443.
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