会议专题

Clay mineral assemblages of terrestrial records (Xining Basin, China) during the Eocene-Oligocene climate Transition (EOT) and its environmental implications

  The global climate cooling, from ”greenhouse” to ”icehouse”, during Eocene-Oligocene Transition (EOT) is one of the great events during Cenozoic climate deterioration (Zachos et al., 2001; Lear et al., 2008).It was accompanied by the expansion of ice sheets on the Antarctic continent (Coxall et al., 2005), a declining of atmospheric CO2 Concentration (Pearson et al., 2009), a global sea-level drop (Katz et al., 2008), and a biotic reorganization (Hansen et al., 2004).

Clay mineral assemblage EOT terrestrial record China

Chun-Xia Zhang Zheng-Tang Guo

Key Laboratory of Cenozoic Geology and Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China

国内会议

帕纳科第12届用户X射线分析仪器技术交流会

杭州

英文

123-124

2012-09-01(万方平台首次上网日期,不代表论文的发表时间)