本文選題：四川省阿壩州 + 阿梢垴遺址��； 參考：《考古》2017年10期

【摘要】：正九寨溝地處四川盆地向青藏高原過渡的邊緣地帶,屬高山峽谷地貌區(qū)。溝內(nèi)地勢南高北低,相對高差達(dá)2768米。在溝內(nèi)高半山地帶,分布有階梯狀的小型黃土階坎(Terracette)。四川大學(xué)九寨溝聯(lián)合實驗室曾對九寨溝內(nèi)階坎地貌的形成機(jī)制進(jìn)行了初步探討,認(rèn)為其很可能與古今人類的生產(chǎn)活動密切相關(guān)[1]。經(jīng)過廣泛踏查,最終在古洼寨、尖盤寨、扎如寨附近發(fā)現(xiàn)了古代遺址的線索,其中以阿梢垴遺址堆積最為豐富(圖
[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.
【作者單位】： 四川大學(xué)考古學(xué)系;四川省阿壩藏族羌族自治州文物管理所;九寨溝管理局科研處;阿壩州文管所;
【基金】：國家社科基金項目“青藏高原及周鄰區(qū)域史前考古學(xué)文化比較研究(14BKG005)” 九寨溝環(huán)境可持續(xù)發(fā)展國際聯(lián)合實驗室項目 教育部人文社科項目“青藏高原絲綢之路考古調(diào)查與研究”(16JJD780011)資助
【分類號】：K878
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本文編號：2054718