四川阿坝州九寨沟阿梢垴遗址的调查与试掘

发布时间：2018-06-22 23:38

  本文选题：四川省阿坝州 + 阿梢垴遗址　； 参考：《考古》2017年10期

【摘要】：正九寨沟地处四川盆地向青藏高原过渡的边缘地带,属高山峡谷地貌区。沟内地势南高北低,相对高差达2768米。在沟内高半山地带,分布有阶梯状的小型黄土阶坎(Terracette)。四川大学九寨沟联合实验室曾对九寨沟内阶坎地貌的形成机制进行了初步探讨,认为其很可能与古今人类的生产活动密切相关[1]。经过广泛踏查,最终在古洼寨、尖盘寨、扎如寨附近发现了古代遗址的线索,其中以阿梢垴遗址堆积最为丰富(图
[Abstract]:Jiuzhaigou is located in the marginal zone of the transition from the Sichuan basin to the Qinghai Tibet Plateau, which belongs to the alpine valley landform area. The ravine terrain is low in the South and the relative height is 2768 meters. In the high half of the valley, the small scale of the Loess terraced scale (Terracette) is distributed in the high half of the valley. The formation mechanism of the Jiuzhaigou order in the Jiuzhaigou Joint Laboratory of the Sichuan University has been formed. A preliminary discussion is carried out, and it is considered that it is very likely to be closely related to the production activities of ancient and modern human beings. [1]. has been extensively investigated, and finally found the clues of ancient ruins near the ancient depression, the Jian Pan village and the Zhan Zhai village.
【作者单位】： 四川大学考古学系;四川省阿坝藏族羌族自治州文物管理所;九寨沟管理局科研处;阿坝州文管所;
【基金】：国家社科基金项目“青藏高原及周邻区域史前考古学文化比较研究(14BKG005)” 九寨沟环境可持续发展国际联合实验室项目 教育部人文社科项目“青藏高原丝绸之路考古调查与研究”(16JJD780011)资助
【分类号】：K878
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本文编号：2054718