祁连山东段童子坝河阶地对气候变化与新构造运动的响应*
钟岳志1, 李有利1, 熊建国1,2, 雷惊昊1, 辛伟林1, 胡秀1, 刘飞1

Terraces of the Tongziba River, eastern Qilian Mountain and their responses to neotectonic movement and climate change
Zhong Yuezhi1, Li Youli1, Xiong Jianguo1,2, Lei Jinghao1, Xin Weilin1, Hu Xiu1, Liu Fei1
祁连山东段童子坝河下切时段与其他古气候记录对比 a—东居延泽古湖孢粉A/C比( Herzschuh et al .,2004 );b—东居延泽古湖湿度重建( Herzschuh et al .,2004 );c—亚洲冰进记录(每行色块出自同一篇文献: Zhou et al .,1991 ; Lehmkuhl,1997 ; Seong et al ., 2009 ; Nazarov et al .,2012 ; Dortch et al .,2013 ; Murari et al ., 2014 );d—北大西洋冰筏(IRD,ice￣rafted debris)记录中的染色赤铁矿在岩屑颗粒中的百分含量(HSG,hematite￣stained grains; Bond et al ., 2001 ); e—格陵兰氧同位素曲线