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| 中国的黄土与风尘堆积 | |
| 引用本文： | 刘东生,安芷生,袁宝印.中国的黄土与风尘堆积[J].第四纪研究,1985,6(1):113-127. |
| 作者姓名： | 刘东生 安芷生 袁宝印 |
| 作者单位： | 1. 中国科学院地质研究所; 2. 中国科学院地球化学研究所 |
| 摘 要： | 中国的黄土,连同沙漠、戈壁大致位于北纬35-45°范围之内,在华北从西到东形成一个连续的带,这个带基本上分布于中亚的干早半干旱区的南部。中国北部,干旱型的粉砂质黄土主要分布在祁连山、秦岭、泰山和鲁山等山的北翼,形成大规模的黄土高原。 |
EOLIAN PROCESS AND DUST MANTLE(LOESS) IN CHINA |
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| Institution: | 1. Institute of Geology, Academia Sinica, Beijing; 2. Institute of Geochemistry, Academia Sinica, Guiyang |
| Abstract: | Distributional patterns, environmental characteristics and stratigraphical structures of loess in China are discussed. Loess and paleosol occurred alternately during the Quaternary period in northern China. A paleocIimatic curve is proposed and correlated with the paleoclimatic curve of deep sea cores V28-238 tentatively. |
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