摘要
根据黄土剖面中古土壤系列与砂质黄土中常量元素氧化物含量基本特征,主要地质特征、黄土堆积与古土壤形成古气候环境、演化过程与主要元素组分特征、关系进行了讨论,结合孢粉测年等资料,1.19MaB.P.黄土形成以来的气候演变过程与元素组分变化关系。
Based on the oxide content of macroelements in paleosoil and sandy loess, maingeological features and sporopollen data along the loess profile, the paleoclimate environment of 1. 19Ma.B.P. when the loess formed and its evolution later on, and the relationship between paleoclimateevolution and variation of element content have been described.
