Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Suo-Fei Xiong"'
Publikováno v:
Geofluids, Vol 2019 (2019)
The Wushan copper polymetallic deposit is located in the Tongbai-Dabie orogenic belt in central China. Two small granitoid stocks (Donggushan and Xigushan) occur in the deposit, which is next to the largest Qijianfeng Granite Complex in the Suizao ar
Externí odkaz:
https://doaj.org/article/32a266c468374d2f8d417e7dac39ece6
Publikováno v:
Geofluids, Vol 2018 (2018)
The Fuzishan Cu-Mo deposit is located in the Edong district of the Middle-Lower Yangtze River Metallogenic Belt, China. The orebodies mainly occurred as lenticular and bedded shapes in the skarn zone between the Lower Permian Qixia Formation carbonat
Externí odkaz:
https://doaj.org/article/5c41189fcaf54ef3a206a025877f0e95
Publikováno v:
Geofluids, Vol 2017 (2017)
The Nanmushu carbonate-hosted Zn-Pb deposit is located in the Mayuan district of Shaanxi Province, a newly discovered metallogenic district next to the Sichuan Basin, in the northern margin of the Yangtze Block, which is the largest and the only one
Externí odkaz:
https://doaj.org/article/b4b35d340b0e489a9de6f29fc83224df
Publikováno v:
Geofluids, Vol 2017 (2017)
The Liyuan gold deposit is hosted within Archean basement metamorphic rocks and controlled by the NNE-trending faults in the central North China Craton. The ore-forming processes can be divided into three stages (early, middle, and late). Three types
Externí odkaz:
https://doaj.org/article/e9411a6b12624b8cadc5cacd3cd59b65
Publikováno v:
Geofluids, Vol 2017 (2017)
The Zhijiadi Ag-Pb-Zn deposit is located in the central North China Craton. Fluid inclusions (FIs) studies indicate three types of FIs, including aqueous, aqueous-carbonic, and daughter mineral-bearing multiphase inclusions. The daughter minerals in
Externí odkaz:
https://doaj.org/article/f9d03cd0c3884da88d29ca07dc4be5da
Publikováno v:
Mineralium Deposita. 57:1449-1468
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a966ed0567709d26976903da2444b632
https://doi.org/10.1007/s00126-022-01114-2
https://doi.org/10.1007/s00126-022-01114-2
Autor:
Suo-Fei Xiong, Shao-Yong Jiang, Zuo-Hao Chen, Jian-Xin Zhao, Ying Ma, Di Zhang, Zhen-Peng Duan, Pan-Pan Niu, Yao-Ming Xu
Publikováno v:
GSA Bulletin. 134:2880-2890
The ages of Zn-Pb deposits are exceptionally challenging to determine owing to the lack of suitable mineral chronometers and techniques. Here we present the first result for in situ LA-ICP-MS U-Pb dating of carbonates and barite from a Mississippi Va
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5382c038234dd258555aede61ade92a4
https://doi.org/10.1130/b36289.1
https://doi.org/10.1130/b36289.1
Publikováno v:
Precambrian Research. 393:107088
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c567fbb8068e5454a97c77950a739604
https://doi.org/10.1016/j.precamres.2023.107088
https://doi.org/10.1016/j.precamres.2023.107088
Autor:
Shao-Yong Jiang, Run-Sheng Chen, Ying Ma, Xue-Xie Li, Suo-Fei Xiong, Hartwig E. Frimmel, Lü-Yun Zhu
Publikováno v:
Mineralium Deposita. 57:13-34
The large Hebaoshan gold deposit (41.5 t Au, average grade: 3.5 g/t) is located in a hitherto poorly documented gold province in the northeastern part of the South China Block. It is hosted by Precambrian metasedimentary rocks that experienced Triass
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::68f507e61235ceef996130a09aa3f455
https://doi.org/10.1007/s00126-021-01046-3
https://doi.org/10.1007/s00126-021-01046-3
Publikováno v:
Gondwana Research. 91:231-253
The Shuangqishan gold deposit (>20t gold) is located in a hitherto poorly-documented gold province in the southeastern Cathaysia Block, South China. It is hosted by Neoproterozoic amphibolite-facies metamorphic rocks and consists of quartz-sulfide ve
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::031bab5eb927c70cd13eebe783843b9d
https://doi.org/10.1016/j.gr.2020.11.014
https://doi.org/10.1016/j.gr.2020.11.014