| 摘要: |
| 于1992年5—6月在南黄海海底打捞到大量海底砾石。通过对这些砾石的形态和表面特征的研究,结合其它证据,发现其形成原因可能与冰期低海面时期陆架上的风力作用有关,因此将这些砾石命名为“风成砾石”。 |
| 关键词: 风成砾石 风力作用 冰期 |
| DOI： |
| 分类号: |
| 基金项目:中国科学院海洋研究所调查研究报告第2208号。国家“八五”攻关项目—南黄海陆架勘查课题,85-904-0l号 |
附件 |
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| THE DISCOVERY OF VENTIFACT IN THE SOUTHERN YELLOW SEA |
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Yu Hongjun
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Institute of Oceanology, Academia Sinica, Qingdtto, 266071
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| Abstract: |
| Careful study of many stones collected by bottorntrawl in June, 1992 by the “RV Scinece I” of the Institute of Oceanology, Academia Sinica, during investigations in the (southern) Yellow Sea continental shelf showed they were composed of sandstone (sandy gravel) and probably resulted from eolion erosion in the glacial period. These stones were mostly longish and in cylindrical form, and showed many signs of abrasion by wind, for which reason they are called “ventifacts”. |
| Key words: Ventifact, Eolion erosion, Glacial period |
