Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Weice Zhao"'
Publikováno v:
International Journal of Earth Sciences. 112:1251-1275
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::416db30139d8ff495c3d5fd679468dad
https://doi.org/10.1007/s00531-023-02303-8
https://doi.org/10.1007/s00531-023-02303-8
Autor:
Bo Feng, Hao Xing, Xiaobo Zhao, Chunji Xue, Ling Xing, Weice Zhao, Weizhong Yang, David T. A. Symons
Publikováno v:
International Journal of Earth Sciences. 111:2715-2739
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c98090a1d33a2dd230d2c78a2f4d3e12
https://doi.org/10.1007/s00531-021-02139-0
https://doi.org/10.1007/s00531-021-02139-0
Autor:
Reimar Seltmann, Jens C.Ø. Andersen, Chunji Xue, Xiaobo Zhao, Ling Xing, Xinjie Cui, Weice Zhao, Alla Dolgopolova
Publikováno v:
Geological Society, London, Special Publications. 516:155-176
The western Tianshan Gold Belt hosts numerous giant and large gold deposits that have been formed during the late Paleozoic amalgamation of the Tianshan orogen. However, little is known about their exhumation histories during the Mesozoic to Cenozoic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75c9245cbc04bd80fc0bf8cde8fcfd28
https://doi.org/10.1144/sp516-2020-201
https://doi.org/10.1144/sp516-2020-201
Publikováno v:
Ore Geology Reviews. 107:888-902
The western Tianshan orogen is one of the world’s most important gold provinces. It hosts numerous world-class gold deposits along the southern and northern margins of the Middle Tianshan. Most deposits occur within large-scale fault zones and/or d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f28e4e8b6d2202e61831f0903a6d86c5
https://doi.org/10.1016/j.oregeorev.2019.03.028
https://doi.org/10.1016/j.oregeorev.2019.03.028
Autor:
Xiaobo Zhao, Weice Zhao, David T. A. Symons, Reimar Seltmann, Chunji Xue, Yong Zhang, Alla Dolgopolova
Publikováno v:
Journal of the Geological Society. 178
Epithermal gold deposits are rarely well preserved in pre-Mesozoic terranes because of their low-temperature mineralization at shallow crust levels, and they are easily destroyed by subsequent erosion or depleted by tectonic events. However, several
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2b5ce2a24cf1b468e3b55f7a0614f1f2
https://doi.org/10.1144/jgs2020-099
https://doi.org/10.1144/jgs2020-099