Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Shun-da Li"'
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
The Haerdaban Pb-Zn deposit is located on the western edge of the Chinese Western Tianshan Orogen. This deposit consists of stratiform and veined mineralization hosted in Proterozoic carbonaceous and dolomitic limestone. Three metallogenic stages wer
Externí odkaz:
https://doaj.org/article/b26efe665d4e45c1afce106408845ff2
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
The Jinba gold deposit is located in the Maerkakuli Shear Zone of the south Altay Orogenic Belt, NW China. Mineralization types are classified as altered rock–and quartz vein–type. Orebodies occur as veins or lenses controlled by NW–trending fa
Externí odkaz:
https://doaj.org/article/7fe018043c334d54a7e6c447070073b9
Autor:
Xue-Bing Zhang, Feng-Mei Chai, Chuan Chen, Hong-Yan Quan, Ke-Yong Wang, Shun-Da Li, Shi-Shan Wu
Publikováno v:
Minerals, Vol 10, Iss 7, p 584 (2020)
Eastern Tianshan hosts a number of porphyry Cu deposits. However, these mainly formed in the Jueluotage Belt, in the middle part of Eastern Tianshan. The Tonggou porphyry Cu mineralization is an exception to this, since it is located in the Bogda Oro
Externí odkaz:
https://doaj.org/article/8162ec36f9c944e0bc0321fce5a0b8f8
Publikováno v:
Minerals, Vol 9, Iss 7, p 394 (2019)
The Qibaoshan polymetallic ore field is located in the Wulian area, Shandong Province, China. Four ore deposits occur in this ore field: the Jinxiantou Au−Cu, Changgou Cu−Pb−Zn, Xingshanyu Pb−Zn, and Hongshigang Pb−Zn deposits. In the Jinxi
Externí odkaz:
https://doaj.org/article/f2c64fc1b2e440b98726ef5c72d20d63
Publikováno v:
Minerals, Vol 8, Iss 10, p 448 (2018)
The Jinchang gold deposit is located in the eastern Yanji–Dongning Metallogenic Belt in Northeast China. The orebodies of the deposit are hosted within granite, diorite, and granodiorite, and are associated with gold-mineralized breccia pipes, diss
Externí odkaz:
https://doaj.org/article/00362c1ed1b54d54872b279819803f88
Publikováno v:
Geological Magazine. 158:271-294
Most skarns are found near the pluton or in lithologies containing at least some limestone. However, recent research has shown that neither a pluton nor limestone is necessarily required to form a skarn deposit. The newly discovered Bagenheigeqier Pb
Publikováno v:
Journal of Geochemical Exploration. 200:167-180
The southern Great Xing'an Range (SGXR) is one of the most important metallogenic belts in Northeast China, containing numerous deposits of Cu, Fe, Pb, Zn, Au, etc. The newly discovered Shenshan Fe–Cu skarn deposit, located in the northern segment
Publikováno v:
Ore Geology Reviews. 107:735-753
Whether multiple mineralization styles in porphyry deposits are the result of one or multiple pulses of magmatism is unknown. In this paper, we present new age and geochemical data on the Jinchang porphyry gold-copper (Au-Cu) deposit, an important de
Autor:
Shun-Da Li, Xuebing Zhang, Hong-yan Quan, Shi-Shan Wu, Chuan Chen, Feng-Mei Chai, Keyong Wang
Publikováno v:
Minerals
Volume 10
Issue 7
Minerals, Vol 10, Iss 584, p 584 (2020)
Volume 10
Issue 7
Minerals, Vol 10, Iss 584, p 584 (2020)
Eastern Tianshan hosts a number of porphyry Cu deposits. However, these mainly formed in the Jueluotage Belt, in the middle part of Eastern Tianshan. The Tonggou porphyry Cu mineralization is an exception to this, since it is located in the Bogda Oro
Publikováno v:
Journal of Asian Earth Sciences. 165:241-255
The Bianbianshan Cu-polymetallic deposit is located in the Xilamulun Cu-Mo belt of Inner Mongolia, NE China, and occurs within Late Jurassic andesite, rhyolite and tuff. Cu mineralization is observed in various types of hydrothermal disseminated vein