摘要
据近年来福建沿海大陆架和相邻的浙江宁波发现的晚更新世海相、海-陆过渡相地层和新构造期活动断裂的研究成果,对前人提出的福建台湾晚更新世存在陆桥之说进行探讨。
According to the recent researchs on the coastal continental shelf of Fujian Province and the Late Pleistocene marine, marine-continental factes strata and the neotectonic active fancied structures found in the Ningbo area, Zhejiang Province, the author made a discussion on whether a land bridge was in existence between Fujian and Taiwan Provincs in the Late Pleistocene Epoch. It is concluded that there was not a land bridge between Fujian and Taiwan Provinces in the Late Pleistocene Epoch.
出处
《福建地质》
1998年第4期214-220,共7页
Geology of Fujian
关键词
陆桥
晚更新世
福建
台湾
地层
land bridge, Late Pleistocene, Fujian Province, Taiwan Province