A luminescence dating study of the sediment stratigraphy of the Lajia Ruins in the upper Yellow River valley, China

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• 作者：Yuzhu Zhang ; Chun Chang Huang ; ^{cchuang@snnu.edu.cn" class="auth_mail} ; Jiangli Pang ; Yali Zhou ; Xiaochun Zha ; Longsheng Wang ; Liang Zhou ; Yongqiang Guo ; Leibin Wang
• 关键词：Yellow River ; Guanting Basin ; Lajia Ruins ; Qijia Culture ; OSL
• 刊名：Journal of Asian Earth Sciences
• 出版年：15 June, 2014
• 年：2014
• 卷：87
• 期：Complete
• 页码：157-164
• 全文大小：3340 K

文摘

Pedo-sedimentological fieldwork were carried out in the Lajia Ruins within the Guanting Basin along the upper Yellow River valley. In the eolian loess-soil sections on the second river terrace in the Lajia Ruins, we find that the land of the Qijia Culture (4.20-3.95 ka BP) are fractured by several sets of earthquake fissures. A conglomerated red clay covers the ground of the Qijia Culture and also fills in the earthquake fissures. The clay was deposited by enormous mudflows in association with catastrophic earthquakes and rainstorms. The aim of this study is to provide a luminescence chronology of the sediment stratigraphy of the Lajia Ruins. Eight samples were taken from an eolian loess-soil section (Xialajia section) in the ruins for optically stimulated luminescence (OSL) dating. The OSL ages are in stratigraphic order and range from (31.94 卤 1.99) ka to (0.76 卤 0.02) ka. Combined OSL and ¹⁴C ages with additional stratigraphic correlations, a chronological framework is established. We conclude that: (1) the second terrace of the upper part of Yellow River formed 35.00 ka ago, which was followed by the accumulation of the eolian loess-soil section; and (2) the eolian loess-soil section is composed of the Malan Loess of the late last glacial (MIS-2) and Holocene loess-soil sequences.