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| 乌鲁木齐仓房沟晚更新世地层及沉积环境的初步研究 | |
| 引用本文： | 韩淑媞,叶玮.乌鲁木齐仓房沟晚更新世地层及沉积环境的初步研究[J].第四纪研究,1986,7(2):87-95. |
| 作者姓名： | 韩淑媞 叶玮 |
| 作者单位： | 1. 新疆大学地理系; 2. 中国科学院新疆分院地质研究所 |
| 摘 要： | 仓房沟晚更新世沉积物分布于乌鲁木齐市西南, 乌库公路九公里牌附近妖魔山南坡脚下。仓房沟是一条由东北流向西南的泉水沟, 属乌鲁木齐河西侧的一条支流。 |
STUDIES OF THE LATE PLEISTOCENE STRATA AND THE SEDIMENTARY ENVIRONMENT IN CANGFANOGOU, NEAR URUMUQI |
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| Institution: | 1. Department of Geography, University of Xinjiang; 2. Institute of Geography, Academy Sciences of Xinjiang |
| Abstract: | According to the studies of fossiI mammalia, sporopollen analysis, and sedimentarycharacteristics, such as grain-ssize, heavy minerals, geoehemistry and so on, the Cang-fanggou formation which consists of alternating cobble, pebble, silt and sandy clay, canbe divided into three members, the upper, the middle and the lower, which reflect ,hedififerent dynamic conditions and sedimentary environments. |
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