Zobrazeno 1 - 10
of 103
pro vyhledávání: '"Fengyue Sun"'
Publikováno v:
Minerals, Vol 12, Iss 9, p 1085 (2022)
The Ela Mountain area is located at the easternmost point of the East Kunlun Orogen, in which voluminous igneous rocks developed in the Triassic period, and it is a good place to investigate the tectonic evolution of the Paleo-Tethys Ocean. In this s
Externí odkaz:
https://doaj.org/article/dd83dbdcb5ba4626b0374f40ed7013c7
Autor:
Zhongcui Pan, Fengyue Sun, Zhichao Cong, Nan Tian, Wei Xin, Li Wang, Yajing Zhang, Dongqian Wu
Publikováno v:
Minerals, Vol 12, Iss 7, p 880 (2022)
The East Kunlun Orogenic Belt is located in the western part of the Central Orogenic Belt of China, with a large number of Triassic igneous rocks parallel to the Paleo-Tethys ophiolite belt, which provides a large amount of geological information for
Externí odkaz:
https://doaj.org/article/16e3b4a96609412fa216aa6987edf229
Autor:
Liang Li, Haotian Liu, Changbing Wang, Fengyue Sun, Kai Zhang, Chengcheng You, Yonggang Sun, Shucheng Tan
Publikováno v:
Geofluids, Vol 2021 (2021)
A study of ore-forming fluid geochemistry and S-H-O isotopes has been conducted to reveal the metallogeny of the Dagangou Au-Ag-Cu-Sb deposit, NW China. Three mineralization stages are identified within Dagangou, including ankerite-quartz-pyrite (Ank
Externí odkaz:
https://doaj.org/article/9ad9c58406764ec8bd25b3fbd27d322e
Publikováno v:
Minerals, Vol 10, Iss 12, p 1136 (2020)
The Hutouya polymetallic skarn deposit lies in the Qimantagh area of the East Kunlun Orogenic Belt, NW China. Skarnization and mineralization at the deposit are closely associated with contemporary felsic intrusions. In this paper, zircon U-Pb ages a
Externí odkaz:
https://doaj.org/article/5007f8262ad24b9a8a0ad0711f1f21c1
Autor:
Liang Li, Fengyue Sun, Huiwen Liu, Shucheng Tan, Lu Yu, Fei Wang, Dali Shen, Xueping Wang, Yonggang Wang
Publikováno v:
Minerals, Vol 10, Iss 10, p 837 (2020)
The Niubiziliang Ni-(Cu) deposit is the first magmatic Ni-Cu sulfide deposit in the North Qaidam Orogenic Belt (NQOB), NW China, and plays a significant role in geological evolution, Ni-Cu mineralization, and exploration in the NQOB. Here, we report
Externí odkaz:
https://doaj.org/article/950e7337e69049eb9d01dd6be96b92e1
Publikováno v:
Minerals, Vol 9, Iss 5, p 275 (2019)
The Akechukesai IV mafic−ultramafic complex, located in the western segment of the eastern Kunlun orogenic belt (EKOB), represents a newly-discovered complex, containing Ni ores at grades of up to 0.98% Ni. It is dominated by olivine pyroxenite, py
Externí odkaz:
https://doaj.org/article/1dd5a0532c7841b2a0284387d42a2145
Publikováno v:
Journal of Colloid and Interface Science. 645:188-199
Autor:
Changle Yue, Na Liu, Yaping Li, Yang Liu, Fengyue Sun, Wenjing Bao, Yongxiao Tuo, Yuan Pan, Ping Jiang, Yan Zhou, Yukun Lu
Publikováno v:
Journal of Colloid and Interface Science. 645:276-286
Publikováno v:
Gondwana Research. 115:37-56
Publikováno v:
International Geology Review. :1-21