古元古代大氧化事件(GOE)前后海洋环境的变化: 来自华北条带状铁建造(BIF)岩相学和地球化学的证据*
张连昌1,2, 兰彩云3, 王长乐1,2, 彭自栋1,2, 佟小雪1,2, 李文君1,2, 董志国1,2

Changes of oceanic environment before and after the Paleoproterozoic Great Oxidation Event(GOE): Evidence from petrography and geochemistry of banded iron formation(BIF)from the North China Craton
Zhang Lian-Chan1,2, Lan Cai-Yun3, Wang Chang-Le1,2, Peng Zi-Dong1,2, Tong Xiao-Xue1,2, Li Wen-Jun1,2, Dong Zhi-Guo1,2
华北克拉通条带状铁建造中 δ 56Fe同位素组成及全球对比(改自 Bekker et al ., 2010 )