摘要
本文应用区域分析的方法,着重从地质构造、气候和水文状况、历史因素三方面分析了福州南台岛由一个面积较小的岩石岛,演变为一个面积较大的半岩半沙的岛连岛的发展过程。
This paper tries to investigate the formation process of Nantai island in Fuzhou by the regional analysis of geological structure, hydrological condition and historicail factors. It shows that Nantai island has once existed in several small rock islands which fiery are tied in a large island composed of half rock and half sahd.
出处
《福建师范大学学报（自然科学版）》
CAS
CSCD
1989年第4期97-102,共6页
Journal of Fujian Normal University：Natural Science Edition
关键词
福州
南台岛
区域分析法
演变
Nantai island of Fuzhou, regional analysis, geological structure, hydrological condition, formation of island
