A New Model for Correlation between the Marine Benthic Oxygen Isotope and Red Clay Magnetic Susceptibility on the Chinese Loess Plateau
A New Model for Correlation between the Marine Benthic Oxygen Isotope and Red Clay Magnetic Susceptibility on the Chinese Loess Plateau
复制标题
黄土高原海洋底栖氧同位素与红土磁化率关联新模型
DOI：
10.1111/1755-6724.13344
复制
发表时间：
2017-06
影响因子：
3.3
通讯作者：
Yue Leping
中科院分区：
文献类型：
--
作者：
Gong Hujun;Zhang Rui;Zhang Yunxiang;Yue Leping
本文建立了中国黄土高原海洋底栖动物氧同位素与红粘土磁化率的相关模型。题目包括：中国黄土高原风成沉积物中发现的晚新生代古气候变化的大陆档案；红粘土磁化率；黄土高原3个剖面的质谱曲线呈现总体趋势；并且可能形成红粘土的条件增加了季风降水。
The article presents a model for correlation between the Marine Benthic Oxygen Isotope and Red Clay Magnetic Susceptibility on the Chinese Loess Plateau. Topics include continental archives of palaeoclimate change in the Late Cenozoic found in Aeolian sediments on the Chinese Loess Plateau; magnetic susceptibility (MS) of red clay; a general trend found in MS curves from three sections on Loess Plateau; and possible formation of red clay conditions of increasing monsoonal precipitation.