Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Huaide Chen"'
Autor:
Huaide Chen, Guojun Xu, Chenxin Jin, Jize Wu, Linwu Xiong, Xiaomin Li, Fugen Sun, Lang Zhou, Zhihao Yue
Publikováno v:
Materials Letters. 341:134192
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7e0a774fadb023eeb6c2013493527722
https://doi.org/10.1016/j.matlet.2023.134192
https://doi.org/10.1016/j.matlet.2023.134192
Autor:
Yongshou Li, Tong Pan, Hongpu Li, Huaide Cheng, Pengcheng Zhang, Wenhua Han, Binkai Li, Qin Yuan, Xuehai Ma, Haizhou Ma
Publikováno v:
Frontiers in Environmental Science, Vol 11 (2024)
Ca-Cl brine is a highly mineralized special water body occurring in oceanic ridges or basins. The deep part of the western Qaidam Basin is rich in Ca-Cl brine, which is essential for the formation of (MgSO4-deficient) potash deposits. Previous studie
Externí odkaz:
https://doaj.org/article/490d24a3d2e24a388c7d6f6415b03d27
Publikováno v:
Geofluids, Vol 2023 (2023)
The reserves of nitrate (NO3-) mineral resources in the Turpan-Hami Basin in Xinjiang rank second after those in the Atacama Desert in Chile, South America. Considerable attention has been devoted to nitrogen (N) sources of NO3- deposits in recent ye
Externí odkaz:
https://doaj.org/article/de2f0075ed1d42c0af99699bb5a5cfd7
Autor:
Xiwei Qin, Haizhou Ma, Xiying Zhang, Xiasong Hu, Guorong Li, Huaide Cheng, Jibin Han, Yongshou Li, Weiliang Miao, Wenhua Han, Sha Yang, Qian Song, Mei Wu
Publikováno v:
Geofluids, Vol 2022 (2022)
The Nangqen and Qamdo (NQ-QD) basins in China have very rich geothermal and brine resources. The origin and spatiotemporal evolutionary processes of its hot and saline springs however remain unclear. Geochemical and isotopic (18O, 2H, 3H) studies hav
Externí odkaz:
https://doaj.org/article/25fdbc2516bf416fa08a035144ee8244
Autor:
Xiaolong Yuan, Fanwei Meng, Xiying Zhang, Jinchang Sheng, A. R. Galamay, Huaide Cheng, Yongshou Li, Weiliang Miao, Wenxia Li, Qiliang Tang, Jun Li, Yongsheng Du
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Polyhalite occurrence in the Kunteyi Playa in the Qaidam Basin has been known for many years. However, the genetic mechanism of this deposit remains unclear. In this study, a typical section in the playa depocenter is selected to study the polyhalite
Externí odkaz:
https://doaj.org/article/27ca7645d4734e8b93b7ea68a9b8c0b5
Publikováno v:
Geofluids, Vol 2019 (2019)
An average of concentrations of Na+, Mg2+, Ca2+, K+, and Cl– in fluid inclusions, from the Khorat Plateau evaporite primary halite, was employed. The evaporation–crystallization sequence and paths were obtained under various temperature condition
Externí odkaz:
https://doaj.org/article/d5c3b7737fb844dc8c11b012d1a814f9