对边缘地带论的发展:“断裂带”分析  

Development of the Rimland Theory: “Fracture Zone”Analysis

作　　者：齐尚才 江帆[1] 

机构地区：[1]广西大学政治学院,广西南宁530004

出　　处：《西南交通大学学报（社会科学版）》2015年第4期92-100,共9页Journal of Southwest Jiaotong University(Social Sciences)

摘　　要：早期地缘政治学家马汉、麦金德、斯派克曼等确立了地缘政治理论的基本要素,而他们以后的主要学者(如布热津斯基、亨廷顿等)则大多背离了这些要素,因而其理论充满了不确定性和矛盾性。要实现地缘政治理论的真正发展,首先必须在传统地缘政治理论基本要素指引下回归斯派克曼边缘地带论,并以边缘地带是一个"缓冲地带"等论点为基础,结合麦金德的心脏理论以及进攻性现实主义相关论点,对边缘地带理论进行重构。边缘地带作为一个缓冲地带,必然存在着稳固地段和断裂地带,边缘地带上的断裂地带将是海权与陆权折冲的关键地带,即未来"地缘政治巨变中心"。Early geographical scientists such as Mahan, Mackinder and others scholars have established the basic elements of the geopolitical theory,while the main scholars after Spykman such as Brzezinski and Huntington have mostly deviated from the traditional analytical paradigm. Their theories are therefore full of uncertainties and contradictions. If we adhere to the research specification of the traditional geopolitical theory,returning to Spykman's Rimland Theory on the basis that the rimland is a'buffer zone'and combing Mackinder's Heart theory and some related arguments of Offensive realism,the Rimland Theory can be refactored. The rimland as a 'buffer zone'must contain the solid and fracture zones. The fracture zone on rimland will be the key areas when sea power and land power confront each other,namely the 'geopolitical upheaval center'in the future.

关 键 词：地缘政治 边缘地带 断裂带分析 地中海—黑海 

分 类 号：D80[政治法律—政治学]