新仙女木期黄河晋陕峡谷古风成沙层年代及其物质来源
张玉柱1,2(
), 黄春长3, 陈莹璐3, 谭志海4, 杨利荣2, 张云翔2, 邱海军1, 刘波1, 赵发珠1
), 黄春长3, 陈莹璐3, 谭志海4, 杨利荣2, 张云翔2, 邱海军1, 刘波1, 赵发珠1
Age and provenance of Younger Dryas paleo-aeolian sandlayers in the Jin-Shaan Gorges of the Yellow River
Yuzhu ZHANG1,2(), Chunchang HUANG3, Yinglu CHEN3, Zhihai TAN4, Lirong YANG2, Yunxiang ZHANG2, Haijun QIU1, Bo LIU1, Fazhu ZHAO1
), Chunchang HUANG3, Yinglu CHEN3, Zhihai TAN4, Lirong YANG2, Yunxiang ZHANG2, Haijun QIU1, Bo LIU1, Fazhu ZHAO1
图2. 黄河晋陕峡谷壶口至龙门段北桑峪晚更新世以来黄土—土壤剖面及其所夹古风成沙层
Fig. 2. The Late Pleistocene and Holocene loess-soil profile containing paleo-aeolian sand layers at theBeisangyu site (BSY) in the Hukou-Longmen reach in the Jin-Shaan Gorges of the Yellow River
