本文選題：西喜馬拉雅 + 克什米爾��； 參考：《考古》2014年12期

【摘要】：正一、引言目前整個西藏高原已經(jīng)確認(rèn)的新石器時代文化有西藏東部以昌都卡若遺址為代表的卡若文化(距今5500~4000年)~([1])、西藏中部以拉薩曲貢遺址為代表的曲貢文化(距今4000~3000年)~([2]);另外,在雅魯藏布江下游的藏東南地區(qū)尚存在一些新石器時代遺址,被稱之為"林芝類型"~([3])。上述藏東和西藏中部的新石器時代晚期考古學(xué)文化都具有強烈的"地方性",文化面貌上仍有很大差異~([4]),應(yīng)與各自所處的生態(tài)區(qū)位關(guān)系密切。西藏西部生態(tài)條件和藏東、藏中迥然有別,迄今除發(fā)現(xiàn)過一系列石器采集地點外,尚未發(fā)現(xiàn)明確屬于
[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.
【作者單位】： 四川大學(xué)中國藏學(xué)研究所;
【基金】：國家社會科學(xué)基金重大招標(biāo)項目(12&ZD151) 教育部人文社科項目(11JJD780006) 四川大學(xué)中央高�；究蒲袠I(yè)務(wù)費專項資金(SKJC201002)資助
【分類號】：K871.13

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