摘要
本文从地形地貌、构造、地层、古文化遗存等方面，阐述台北盆地的形成及环境演变．台北盆地为断陷成因，断陷年代为中更新世末晚更新世初，盆地的发育演变、环境变迁与构造运动（台湾运动之余动）、里斯一玉木间冰期（Q3）及其后的海平面升降波动变化息息相关。
The Taibei basin lies at the northern Taiwan Island, and its morphology is like a triangle.There are Tanshui river drainage system and many ichnofossils in the basin. Based on the analysis of the land form, tectonics, terraces, base level, strata ,environmental archaeology, and other relevant data of itS surroundings i. e. Taiwan Strait, the coast of South China etc, this peper studies the formation, evolution and environmental change of the Taibei basin. The Taibei basin was a fault hem and its fault age was between Q and Q. The evolution and environmental change of the Taibei basin have ben correlated with the tectonic movement after Taiwan MOvement and sea level change since Q.
出处
《热带地理》
北大核心
1997年第1期10-18,共9页
Tropical Geography
基金
国家自然科学基金!49271070
关键词
盆地
形成演变
环境
台北盆地
Taibei basin
Formation and evolution: Environmental archaeology
