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2 金沙江干热河谷华弹段中黄土状土与堰塞湖相沉积的空间分布（A）及河流阶地与黄土状土剖面（B） |
| Fig.2 Spatial distribution of loess-like sediments and dammed lake sediments （A） and river terrace and loess profile （B） in the Huatan section of Jinsha River Valley |
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