| 烟台附近海岸风沙地貌的初步研究 |
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| 引用本文： | 张振克. 烟台附近海岸风沙地貌的初步研究[J]. 中国沙漠, 1995, 15(3): 210-215 |
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| 作者姓名： | 张振克 |
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| 作者单位： | 山东烟台师范学院地理系, 烟台 264025 |
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| 基金项目： | 国家自然科学基金资助项目 |
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| 摘 要： | 在野外调查基础上,对烟台附近海岸风沙分布、风沙地貌类型及地貌发育过程进行了探讨。指出全新世海岸变迁是海岸风沙地貌发育的基础,6000aB.P.以来有5个风沙堆积期,前4个风沙堆积期与4个海平面下降期一致,第5风沙堆积期与小冰期一致。
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| 关 键 词： | 海岸风沙 地貌发育 烟台 |
| 收稿时间： | 1995-02-14 |
STUDY ON THE COASTAL EOLIAN LANDFORM CLOSE TO YANTAI,SHANDONG |
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| Zhang Zhenke. STUDY ON THE COASTAL EOLIAN LANDFORM CLOSE TO YANTAI,SHANDONG[J]. ournal of Desert Research, 1995, 15(3): 210-215 |
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| Authors: | Zhang Zhenke |
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| Affiliation: | Geography Dept.of Yantai Teachers College, Yantai |
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| Abstract: | On the basis of field investigation,the coastal eolian sand distribution,eolian landform types and eolian morphological evolution close to the paralic area of Yantai are discussed.This paper presents that sea level changes are the background of coastal eolian morphological evolution. Since 6000 a B.P.,there have been five periods of eolian sand accumulation(① 5500-4400 a B.P.,② 3600-3000 a B.P.,③ 2500-2000 a B.P.,④ 1400-1000 a B.P.,⑤ 560-130 a B.P.).The preceding four periods were accompanied with four periods of low sea level and the last period was accompanied with the period of Little lce Age. |
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| Keywords: | Coastal eolian sand Morphological evolution Yantai |
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