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	平潭岛岚湖沉积环境和成因的研究; Study on the Sedimentary Environment and Origin of Lanhu Lake in Pingtan Island
	蔡爱智 ; 张金城 ; 李建波 ; 黄建东 ; 石谦 ; 陈丽英
	1996
关键词	沉积环境 风积作用 岚湖 eolian deposition Lanhu Lake sedimentary environment
英文摘要	在中全新世后阶段，当海岸风沙正处于始发状态，平潭西南的岚湖还是一个由多叉的山谷组成的洼地。到全新世晚期，由于全球气候的变化和优势的北北东方向风力的逐渐增强，河谷洼地与海湾相联结的地区长时间受风沙的堆积而形成岚湖。; he paper Focuses on the discussion of sedimentary environment and origin of Lanhu Lake in Pingtan Island.In the late sarge of Middle Holocene, the coastal eolian action in Pingtan Island was in an initial stage and Lanhu Lake on the southwestern part of Pingtan Island was a depression consisting of polyForked valleys.Due to the change of the global climate and gradually strengthened predominant NNE wind in Late Holocene, the eolian sand had been accumulated For a long time in the area between the valley depression and the bay, and Lanhu Lake was Formed.; 国家自然科学基金
语种	zh_CN
内容类型	期刊论文
源URL	[http://dspace.xmu.edu.cn/handle/2288/104643]
专题	海洋环境－已发表论文
推荐引用方式 GB/T 7714	蔡爱智,张金城,李建波,等. 平潭岛岚湖沉积环境和成因的研究, Study on the Sedimentary Environment and Origin of Lanhu Lake in Pingtan Island[J],1996.
APA	蔡爱智,张金城,李建波,黄建东,石谦,&陈丽英.(1996).平潭岛岚湖沉积环境和成因的研究..
MLA	蔡爱智,et al."平潭岛岚湖沉积环境和成因的研究".(1996).

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