Terminal Ediacaran anoxia in deep-ocean: Trace element evidence from cherts of the Liuchapo Formation, South China


Autoria(s): 常华进
Data(s)

2009

Identificador

http://159.226.119.211/handle/311031/48

http://www.irgrid.ac.cn/handle/1471x/73776

Idioma(s)

中文

Fonte

常华进 .Terminal Ediacaran anoxia in deep-ocean: Trace element evidence from cherts of the Liuchapo Formation, South China.Science in China Series D: Earth Sciences ,2009,52(6):807-822

Tipo

期刊论文