Osl dating sand

Marine Geology &Quaternary Geology, 2006, 26(4): 99-104. A review on the research status of forming mechanism of coastaldunes. Earth and Planetary Science Letters, 2010, 29: 171-179.[27] Zhang Jiafu, Mo Dowen, Xia Zhengkai et al.

osl dating sand-32

Building of shore-oblique transverse dune ridges revealed by ground-penetrating radar and opticaldating over the last 500 years on Tottori coast, Japan Sea. 地理学报, 1987, 42(2): 129-141.][40] Chen Fang, Zhu Dakui. Stalagmite δ18O record from Yuhua Cave over the past 500 years and itsregional climate significance. Marine Geology & Quaternary Geology, 2011, 31(3): 117-122. ZHANG Yuzhu, HUANG Chunchang, PANG Jiangli, ZHOU Yali, ZHA Xiaochun, WANG Longsheng, ZHOU Liang.

Geomorphology, 2011, 132(3/4): 153-166.[11] Sawakuchi A O, Kalchgruber R, Giannini P C F et al. 中国科学: B 辑, 1995, 25(2): 211-218.][39] Wu Zheng, Wu Kegang. Dune formation and evolution along the south coastal of Minjiang Estuary. OSL dating of the sediment stratigraphy of the Lajia Ruins in the Guanting Basin in the Upper Yellow River Basin[J].

Within the School of Geography and the Environment, the OLD Laboratory provides support particularly for the Landscape Dynamics research cluster, with a specific focus on low latitude environment and climate change, geoarchaeology and geomorphology.

In addition our researchers continuously engage in efforts to improve and develop the methodology and to further advance our knowledge on the fundamental physical mechanisms underlying the dating method.

Chinese Geographical Science, 2008, 18(3): 255-261.[14] Dong Yuxiang. 中国沙漠, 2011, 31(2): 357-366.][20] Sun Y B, Wang X L, Liu Q S et al. The comparison and analysis of grain size parameters of coastal aeolian sands in China and abroad. 中山大学学报: 自然科学版, 2003, 42(4): 110-113.][35] Ye Yueguang, Diao Shaobo, He Jie. Oceanologia et Limnologia Sinica,1995, 26(5): 488-493.

The coastal aeolian geomorphic type and their distribution pattern in china. 海洋地质与第四纪地质, 2006, 26(4): 99-104.][15] Li Zhiwen, Li Baosheng, Wang Fengnian et al. Impacts of post-depositional processes on rapid monsoon signals recorded by thelast glacial loess deposits of northern China. Acta Scientiarum Naturalium Universitatis Sunyatseni, 2003, 42(4): 110-113.

In this paper, quartz single aliquot regenerative optically-stimulated luminescence (OSL) dating with high resolution sampling was firstly applied to coastal aeolian sand in China for the Anshan (SHA) section (24°36′32.7″ N, 118° 39′ 20.3″ E) near the Anshan archaeological site along the Jinjiang coast, southeast Fujian.

Through grain-size analysis, we assume that the SHA section demonstrates typical coastal aeolian sand characteristics, and affected by the blowout and chemical weathering after coastal sand deposited, the grain size parameter and content of different sizes of fraction have a large change, the grain size become coarser, the sorting for worse.

Luminescence dating of fluvial and coastal red sediments in the SE coast, India,and implications for paleoenvironmental changes and dune reddening. 地理科学, 2012, 32(2): 207-212.][42] Jiang Xiuyang, Li Zhizhong, Shen Chuanzhou et al. A preliminary investigation of historical wind-drift sand along the western coast of the Taiwan Strait. Palaeogeography, Palaeoclimatology, Palaeoecology, 2011, 308(3/4): 492-501.[53] Hu Fangen, Li Zhizhong, Jin Jianhui et al. A 1000-year history of typhoon landfalls in Guangdong, southern China, reconstructed from Chinese historical documentary records.

Tags: , ,