摘要
库孜滚遗址位于新疆维吾尔自治区喀什地区塔什库尔干塔吉克自治县塔什库尔干乡库孜滚村(图一)。遗址位于县城中心东南约12公里的库孜滚沟口,地势西高东低,属于帕米尔高原东部,局部地貌为冰山前缘的洪积台地(图二),地理坐标为北纬37°40′26″、东经75°16′37.22″,海拔3256米。遗址所在地区是塔什库尔干河谷至瓦罕走廊的必经之路。该地区为高原高寒干旱-半干旱气候,海拔高,日照充足,昼夜温差大,降水少。石制品分布范围北起塔吉克新村。
The Kuzigun site excavated in 2018 is uniform in cultural appearance.Nothing but a large number of lithic artifacts spreads out across the ground surface,and in situ cultural layers are only preserved in part of the site.All lithic artifacts,including a variety of simple,chipped stone cores,flakes,as well as reduction byproducts such as broken blocks and debitage,are made from schist.Few tools were found.In addition,blade remains characterized by narrow-face blade core technology are also present.This site,dating to 8000 BP,is the only early Holocene open-air site with reliable stratigraphy and chronology ever found in Xinjiang.It is probably the largest lithic production site among sites of a similar period in China.
出处
《考古》
CSSCI
北大核心
2022年第9期3-13,共11页
Archaeology
基金
北京大学“丝路重大考古发掘与丝路文明传承”项目的资助。
