Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Dong-Tian Wei"'
Autor:
Dong-Tian Wei, Tao-Fa Zhou, Yong Xia, Yu Fan, Zhuo-Jun Xie, Xi-Jun Liu, Qin-Ping Tan, Ling-An Bai, Fang-Yue Wang
Publikováno v:
Ore Geology Reviews. 149:105083
Autor:
Dong-Tian Wei, Tao-Fa Zhou, Yong Xia, Jing Chen, Zhuo-Jun Xie, Xi-Jun Liu, Bao-Cheng Pang, Qin-Ping Tan, Ling-An Bai
Publikováno v:
Ore Geology Reviews. 143:104745
Autor:
Qinping Tan, Yong Xia, Dong-Tian Wei, Zhuojun Xie, Ling’an Bai, Xi-jun Liu, Jeffrey A. Steadman
Publikováno v:
Minerals
Volume 11
Issue 1
Minerals, Vol 11, Iss 2, p 2 (2021)
Volume 11
Issue 1
Minerals, Vol 11, Iss 2, p 2 (2021)
A number of sediment-hosted, Carlin-type/-like gold deposits are distributed in the Youjiang basin of SW China. The gold ores are characterized by high As, Hg, and Sb contents but with low base metal contents (Cu+Pb+Zn <
500&ndash
1000 pp
500&ndash
1000 pp
Publikováno v:
Journal of Asian Earth Sciences. 148:1-12
The Shuiyindong gold deposit is a deeply concealed strata-bound Carlin-type deposit in southwestern Guizhou Province, China. The deposit lies on the eastern limb of the Huijiabao anticline with ores mainly along the anticline axis and hosted in biocl
Publikováno v:
Mineralium Deposita. 52:69-84
The Paiting gold deposit, Guizhou Province, China, has been regarded as a Carlin-type gold deposit by several researchers. Alteration and ore-related minerals from the Paiting deposit were examined, and results were compared with the Cortez Hills Car
Autor:
Yong Xia, Zhuojun Xie, Dong-Tian Wei, Jeffrey A. Steadman, Xi-jun Liu, Qinping Tan, Daniel D. Gregory
Publikováno v:
Ore Geology Reviews. 122:103446
Nibao is a unique thrust fault-controlled and strata-bound disseminated gold deposit in southwestern Guizhou Province, China. In Nibao, pyrite is the major sulfide mineral and Au is structurally bound (Au+) within the pyrite lattice. In this study, w
Publikováno v:
Chinese Journal of Geochemistry. 34:525-539
The Shuiyindong gold deposit is one of the most famous and largest Carlin-type gold deposits in China and is located in southwest Guizhou, in the eastern part of the Huijiabao anticline. The Shuiyindong’s gold mineralization occurred in bioclastic
Autor:
Kohli, Indermeet, Sakamaki, Takeshi, Dong Tian, Wei, Moyal, Dominique, Hamzavi, Iltefat H., Kollias, Nikiforos
Publikováno v:
Photodermatology, Photoimmunology & Photomedicine; Nov2019, Vol. 35 Issue 6, p387-392, 6p
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