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跨喜马拉雅视角下的西藏西部新石器时代

发布时间:2018-05-22 20:28

  本文选题:西喜马拉雅 + 克什米尔 ; 参考:《考古》2014年12期


【摘要】:正一、引言目前整个西藏高原已经确认的新石器时代文化有西藏东部以昌都卡若遗址为代表的卡若文化(距今5500~4000年)~([1])、西藏中部以拉萨曲贡遗址为代表的曲贡文化(距今4000~3000年)~([2]);另外,在雅鲁藏布江下游的藏东南地区尚存在一些新石器时代遗址,被称之为"林芝类型"~([3])。上述藏东和西藏中部的新石器时代晚期考古学文化都具有强烈的"地方性",文化面貌上仍有很大差异~([4]),应与各自所处的生态区位关系密切。西藏西部生态条件和藏东、藏中迥然有别,迄今除发现过一系列石器采集地点外,尚未发现明确属于
[Abstract]:Jung-ichi, In the introduction, the Neolithic culture that has been confirmed throughout the Tibetan plateau at present includes the Karuo culture in eastern Tibet, represented by the Qangdu Karuo site (5500-4000 years ago) and the Qugong culture in central Tibet represented by the Qigong site in Lhasa (40,000 ~ 3000 years ago); in addition, There are still some Neolithic sites in the southeast of Tibet in the lower reaches of the Yarlung Zangbo River, which is called "Linzhi type" ([3]). The archaeological culture of the late Neolithic period in eastern Tibet and central Tibet is strongly "local", and the cultural features are still quite different ([4]), which should be closely related to their ecological location. The ecological conditions in western Tibet are quite different from those in eastern Tibet. Apart from the discovery of a series of stone collection sites so far, it has not been found that there is a definite identity between Tibet and eastern Tibet.
【作者单位】: 四川大学中国藏学研究所;
【基金】:国家社会科学基金重大招标项目(12&ZD151) 教育部人文社科项目(11JJD780006) 四川大学中央高校基本科研业务费专项资金(SKJC201002)资助
【分类号】:K871.13

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