中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Origin, development and evolutionary model of shelf desertization environment in late stage of Upper Pleistocene

文献类型:CNKI期刊论文

作者赵松龄,于洪军,刘敬圃
发表日期1997-04-15
出处Science in China(Series D:Earth Sciences)
关键词shelf desertization, late stage of Upper Pleistocene, dune, loess
英文摘要<正> Based on the study of palaeo-environmental evolution in the shelves of the Eastern China Seas, the concept of "shelf desertization" in the late stage of Upper Pleistocene is defined; the environmental background and evolutionary process of shelf desertization are analysed. Study on the records of subbottom profiling and the data of core samples from shelf areas revealed that during low sea-level stages, the sedimentary environment in the exposed shelf plains was dominated by aeolian depositional process under cold and dry climatic conditions, i.e. under the action of strong winter-monsoon winds. Parts of the exposed marine strata were disintegrated, and aeolian sand dunes were formed on the disintegrated marine deposits, from which the finer sediment grains were blown away by wind and deposited in the downwind areas to form the derivative loess deposits. Thus a desertization environmental system was formed in the exposed shelf plains of the Eastern China Seas.
文献子类CNKI期刊论文
02页:97-104
语种英文;
分类号P534
ISSN号1006-9313
源URL[http://ir.qdio.ac.cn/handle/337002/195167]  
专题中国科学院海洋研究所
作者单位InstituteofOceanology,ChineseAcademyofSciences,Qingdao266071,China ,InstituteofOceanology,ChineseAcademyofSciences,Qingdao266071,China ,InstituteofOceanology,ChineseAcademyofSciences,Qingdao266071,China
推荐引用方式
GB/T 7714
赵松龄,于洪军,刘敬圃. Origin, development and evolutionary model of shelf desertization environment in late stage of Upper Pleistocene. 1997.

入库方式: OAI收割

来源:海洋研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。