摘要
十六国时期中国北方各区域间的地缘关系制约着各族群、各政权的独立发展,使分裂割据之局难以长期维系。在五世纪初河陇雍朔的地缘政治中,关中的后秦与朔方的赫连夏围绕着岭北的对抗是主要矛盾,陇右的西秦与赫连夏的矛盾从属于这一矛盾。陇右、河西间的地缘矛盾又受制于西秦与赫连夏的矛盾。这一重层构造格局的开启与终结均取决于关中政权与关东政权天下之争的结果。后秦在柴壁之战中败于北魏,开启了河陇雍朔的矛盾构造,赫连夏败于北魏则终结了这一矛盾构造。地缘关系的重层构造是推动十六国后期统一趋势形成的重要因素。
The Later Qin occupied guzang and retreated from Hexi three years later.The deep reason is that in the battle of chaibi,it was defeated by the Northern Wei Dynasty and its national strength was insufficient.The power vacuum formed by the retreat of the Later Qin River was filled by the Tufa tribe.The independence of the Tufa tribe led to the rebellion of Shuofang and the restoration of Western Qin in Longyou.The western area of the Later Qin Dynasty was divided into four parts:Guanzhong,Shuofang,Longyou and Hexi.In the geopolitics of that area,the main contradiction was the confrontation between the Later Qin in Guanzhong and Helian Xia in Shuofang around Lingbei,which was subordinate to the contradiction between the Western Qin and Helian Xia in Longyou.The geographical contradiction between Longyou and Hexi was also restricted by the contradiction between the Western Qin and Helian Xia.The opening and ending of this structure depends on the result of the dispute between Guanzhong regime and Guandong regime.The later Qin Dynasty was defeated by the Northern Wei Dynasty in the battle of Chaibi,which opened the contradictory structure of Hexi,Longyou,Yongzhou and Shuofang,and Helian Xia’s defeat in the Northern Wei Dynasty ended this contradictory structure.
出处
《社会科学》
CSSCI
北大核心
2020年第2期150-159,共10页
Journal of Social Sciences
基金
国家民委民族研究项目“十六国北朝时期的中华意识研究”(项目编号:2019-GMB-004)
上海市浦江人才计划项目“中华认同与南北朝时代的国家建构”(项目编号:14PJC030)的阶段性研究成果
关键词
后秦
赫连夏
地缘关系
河陇
雍朔
Later Qin
Helian Xia
Geographical Relationship
He Long
Yong Shuo
