位置：成果数据库 > 会议 > 会议详情页
Overturn of anoxic deep ocean happened at similar to 551 Ma - Evidences from isotopes and trace elem
  • 所属机构名称：中国科学院地质与地球物理研究所
  • 会议名称：8th Annual V M Goldschmidt Conference
  • 成果类型：会议
  • 会场：Vancouver, CANADA
  • 相关项目：新元古代冰期与“雪球地球”假说
作者： Zhang, T.|Chu, X.|Huang, J.|
同会议论文项目
新元古代冰期与“雪球地球”假说
期刊论文 40 会议论文 8
同项目会议论文
华南新元古代江口冰期新的U-Pb年龄限制
C and S isotope records in Doushantuo Formation: Implication for redox fluctuation of the Ediacaran
Carbonate concretions as a window to the evolving chemistry of the early ocean and atmosphere
Terminal Ediacaran oceanic anoxia: Evidence from framboidal pyrites in the cherts of Laobao Formatio
晚新元古代帽碳酸盐岩成因初探
A geochemical redox model for Ediacaran ocean chemistry in Nanhua Basin, South China
Dynamic ocean chemistry around the Marinoan glaciation - Isotopic evidence from cap carbonates