Osl dating of sediments from deserts in northern china
Zircon typological analyses of the major deserts/sand fields in Northern China and its implication for identifying sediment source.Quaternary Sciences, 2013, 33 (2):334~344 高钰涯, 李秋立, 刘 宇等. 第四纪研究, 2016, 36 (5):1015~1026 Gao Yuya, Li Qiuli, Liu Yu et al.Detrital zircon composition of U-Pb ages and Hf isotope of the Hunshandake sandland and implications for its provenance.Acta Petrologica Sinica, 2007, 23 (2):523~528 张瀚之, 鹿化煜, 弋双文等. 第四纪研究, 2013, 33 (2):334~344 Zhang Hanzhi, Lu Huayu, Yi Shuangwen et al.The results show that zircon U-Pb ages of the Hobq Desert sand are mainly distributed around 2.5Ga, 1.9Ga, 960Ma, 450Ma and 280Ma.The zircon age distribution show obvious spatial variation pattern, which reflect eastward decreasing contribution (KD-.6%, KD-.2% and KD-.4%)of 1.4Ga peaks from local sandstone material.U-Pb age framework of the Linzizong volcanic rocks from the Linzhou Basin, Tibet.Quaternary Sciences, 2016, 36 (5):1037~1054 陈发虎, 范育新, 春 喜等. 科学通报, 2008, 53 (10):1207~1219 Chen Fahu, Fan Yuxin, Chun Xi et al.
Science China: Earth Sciences, 2013, 43 (10):1691~1698 何梦颖, 郑洪波, 贾军涛. 第四纪研究, 2013, 33 (4):656~670 He Mengying, Zheng Hongbo, Jia Juntao.
Preliminary research on megalake Jilantai-Hetao in the arid areas of China during the Late Quaternary.
Chinese Science Bulletin, 2008, 53 (10):1207~1219 Wintle A G, Murray A S.
The Hetao paleo-lake may have played an important role in mixing and holding the local source and the Yellow River contribution together for the eastern desert, which may be eroded and contribute the mixed material to the eastern Hobq Desert after its dying.
By contrast, the western desert is sourced more from Yellow River contribution. 水土保持研究, 1998, 5 (3):26~50 Bao Xiaoqing, Chen Quchang.
Totally 900 zircon grains from 9 samples, including 3 surface aeolian sand, 2 lake shore sand, 2 modern river bed sand and 2 Mesozoic sandstone, were collected to correlate the U-Pb ages provenance to trace the possible source of the Hobq Desert.