摘要
将社会科学(文史考古研究)与自然科学(气候变化)结合,分析了黄土高原社会经济发展较长江三角洲地区为早的原因,提出这可能是由于全新世大暖期的气候变化对不同地理区域产生不同的影响,最后并分析了中国历史上的3次移民潮的原因及其对长江三角洲社会经济发展的影响。
This paper is a result of interdisciplinary research between natural and social science.Evidences of more rapid development in the loess plateau than in the Yangtze delta in ancient time are given.It is suggested that this might be due to the fact that Holocene climate warming had different effect on the development of the loess plateau and the Yangtze delta. Finally,causes of three great population migration of the Han People from north China to the lower Yangtze valley are elucidated.The ro1e of three great population migration in rapid economic development of the Yangtze delta since the 7th century is also briefly discussed.
出处
《地球科学进展》
CAS
CSCD
2004年第5期695-698,共4页
Advances in Earth Science
关键词
全新世大暖期
黄土高原
长江三角洲
3次移民潮
Holocene great warm period
The loess plateau
The Yangtze delta
Three great population migration.
