Zobrazeno 1 - 10
of 58
pro vyhledávání: '"Fuyou Chen"'
Publikováno v:
Inorganic Chemistry Frontiers. 10:396-405
We adopted thermal treatment prior to carbonization for Ni-HHTP to open blocked pores and expose multiple active sites. The electronic conductivity, reaction kinetics, specific capacity and stability are enhanced using thermal treatment Ni-HHTP as an
Autor:
Zheng Li, Guojun Jiang, Fuyou Chen, Hui Ma, Yawen Zhao, Zhijuan Sun, Xiangyu Ye, Congjie Gao, Lixin Xue
Publikováno v:
Journal of Hazardous Materials. 452:131332
Publikováno v:
Archaeological and Anthropological Sciences. 14
Autor:
Xingwu Feng, Haibin Wu, Mingchao Shan, Fuyou Chen, Xing Gao, Qin Li, Yinghua Wang, Junyi Ge, John W. Olsen, Ruiping Tang, Xinying Zhou, Yan Li, Chenglong Deng
Publikováno v:
Quaternary Research. 103:113-129
The Dayao Paleolithic site, located in Inner Mongolia on the eastern margin of China's vast northwestern drylands, was a lithic quarry-workshop utilized by Pleistocene human migrants through the region. Determining the age of this activity has previo
Publikováno v:
Antiquity. 95:292-309
Scholars have long debated when the Neolithic began in China. Neolithisation, however, is a process rather than an event. It is more realistic to investigate the timing and nature of the socio-economic trajectory from mobile, microblade-using forager
Publikováno v:
Journal of Membrane Science. 672:121419
Autor:
Jing Zhou, Brian A. Stewart, Xiaomin Wang, Junyi Ge, Feng Li, Yuchao Zhao, Fuyou Chen, Xing Gao
Publikováno v:
Quaternary Research. 103:148-159
A multidisciplinary fieldwork and research project was recently begun at the Yangshang site (220–140 ka), a late Early Paleolithic locale in the western Chinese Loess Plateau. 1696 lithic artifacts and 337 faunal remains were recovered during the e
Publikováno v:
Quaternary International. 535:13-20
The Huangniliang site, located in the coastal province of Shandong, in North China, was excavated in 2013. Optically stimulated luminescence results show that the age of the deposits ranges from 59 to 54 ka, corresponding to the initial part of Marin
Publikováno v:
Review of Palaeobotany and Palynology. 304:104718
Publikováno v:
Separation and Purification Technology. 297:121438