论文摘要
<正>Carbon dioxide draw-down resulting from enhanced chemical weathering during orogenesis has been invoked to explain late Cenozoic global cooling. Establishing chemical weathering records from the India–Asia collision zone is important to test this hypothesis because uplift of the Tibetan Plateau is thought to be responsible for
论文目录
文章来源
类型: 国内会议
作者: Xueping Ren,Junsheng Nie,Joel E.Saylor,Hua Li,Meredith A.Bush,Brian K.Horton
来源: 2019年中国地球科学联合学术年会 2019-10-27
年度: 2019
分类: 基础科学
专业: 地质学
单位: Lanzhou University,University of Houston,Colorado School of Mines
分类号: P512.1
DOI: 10.26914/c.cnkihy.2019.061307
页码: 19
总页数: 1
文件大小: 233k
下载量: 1