金沙江干热河谷华弹段黄土状土的成因、年龄及其古气候指示意义
The genesis， age and its paleoclimatic significance of loess-like sediments in the Huatan section of the dry-hot valley of the Jinsha River
金沙江干热河谷华弹段黄土状土的成因、年龄及其古气候指示意义 |
| 刘芬良, 高红山, 潘保田, 李宗盟 |
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The genesis， age and its paleoclimatic significance of loess-like sediments in the Huatan section of the dry-hot valley of the Jinsha River |
| Fenliang Liu, Hongshan Gao, Baotian Pan, Zongmeng Li |
| 图7 金沙江干热河谷巧家段中黄土状土的发育过程（左为河谷纵剖面视图下的黄土状土发育过程，右为河谷横断面视图下的黄土状土发育过程） |
| Fig.7 Formation model of the loess-like sediments in the Qiaojia section of the Jinsha River Valley. The left column is the development process of loess-like sediments from the river valley longitudinal section view， and the right is the development process of loess-like sediments from the river valley cross section view |
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