MIS 3以来雅鲁藏布江流域风成沉积及环境意义
Aeolian sediments and their paleoenvironmental implication in the Yarlung Zangbo catchment (southern Tibet, China) since MIS3
注：a.米林谷底风沙沉积;b.中下游段发育于山麓的爬坡沙丘;c.河流阶地上发育的厚约2.5 m的黄土;d.拉萨—桑日段河谷北岸低山上发育约10 m厚的多层黄土堆积。
MIS 3以来雅鲁藏布江流域风成沉积及环境意义 |
| 凌智永,靳建辉,吴铎,刘向军,夏敦胜,陈发虎 |
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Aeolian sediments and their paleoenvironmental implication in the Yarlung Zangbo catchment (southern Tibet, China) since MIS3 |
| LING Zhiyong,JIN Jianhui,WU Duo,LIU Xiangjun,XIA Dunsheng,CHEN Fahu |
| 图2 雅江流域风沙沉积与黄土沉积 注：a.米林谷底风沙沉积;b.中下游段发育于山麓的爬坡沙丘;c.河流阶地上发育的厚约2.5 m的黄土;d.拉萨—桑日段河谷北岸低山上发育约10 m厚的多层黄土堆积。 |
| Fig. 2 Sand and loess sediments of the Yarlung Zangbo catchment |
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