Fe-Mo同位素与古海洋化学演化
崔豪1, 周炼2, 李超1*,*, 彭兴芳1, 金承胜1, 石炜1, 张子虎1, 罗根明1, 谢树成1

Iron - Molybdenum Isotopes and the Chemical Evolution of Ancient-Oceans
Cui Hao1, Zhou lian2, Li Chao1,*, Peng Xing fang1, Jin Cheng sheng1, Shi Wei1, Zhang Zihu1, Luo Gen ming1, Xie Shu cheng1
图2 新元古代埃迪卡拉纪陡山沱组二段黑色页岩全岩的δ 56 Fe数据的空间分布。 沉积相：宜昌小风河为浅水台地相；九龙湾为内陆架；湖南石门中岭为陆地边缘；张家界四都坪为斜坡相
Fig. 2 The spatial distribution of whole rock δ 56 Fe data from the black shales of MemberⅡof the Ediacaran Doushantuo Formation Sedimental faces: Xiaofenghe is platform; Jiulongwan is Inner shelf; Zhongling is Shelf margin; Siduping is Slope