Zobrazeno 1 - 10
of 56
pro vyhledávání: '"Lie-meng Chen"'
Autor:
Zhi-hui Dai, Peng Liao, Deng-jun Wang, Sen Lin, He-ping Li, Zhi-an Bao, Ke-jun Hou, Lie-meng Chen, Ting-guang Lan, Can Cui
Publikováno v:
JAAS (Journal of Analytical Atomic Spectrometry); Sep2024, Vol. 39 Issue 9, p2309-2318, 10p
Autor:
Lie-Meng Chen, Peter C. Lightfoot, Jian-Ming Zhu, Fang-Zhen Teng, Qing Duan, Runsheng Yin, Guangliang Wu, Song-Yue Yu, Rui-Zhong Hu
Publikováno v:
Geochimica et Cosmochimica Acta. 353:1-12
Publikováno v:
Acta Geochimica. 42:453-470
Autor:
Yu-Feng Deng, Xie-Yan Song, Wei Xie, Lie-Meng Chen, Song-Yue Yu, Feng Yuan, Peter Hollings, Shuai Wei
Publikováno v:
Economic Geology. 117:1867-1879
The Huangshan-Jingerquan belt in Northwest China is one of the most important orogen-hosted magmatic Ni-Cu sulfide metallogenic belts worldwide. The Huangshandong, Huangshan, and Tulaergen deposits are the three largest Ni-Cu deposits along the belt.
Autor:
Jian Kang, Xie-Yan Song, Ting-Mao Long, Qing-Lin Liang, Stephen J. Barnes, Lie-Meng Chen, De-Xian Li, Qi-Xing Ai, Ya-Lin Gao
Publikováno v:
Economic Geology. 117:1809-1825
The Jinchuan Ni-Cu-platinum group element (PGE) sulfide deposit is one of the world’s major magmatic sulfide deposits. The Jinchuan intrusion originally consists of two independent bodies, named the Western and Eastern intrusions. Recently, an unde
Publikováno v:
Economic Geology. 117:1827-1844
Convergent margins are commonly deemed to have poor potential to form giant magmatic Ni-Cu-(platinum group element) sulfide deposits, due to the possibly low lithospheric geothermal gradient and the small basaltic magma fluxes. This view, however, is
Publikováno v:
Geochimica et Cosmochimica Acta. 308:273-290
To constrain the mechanisms governing the extremely large variations of Mg and Fe isotopes in magmatic Fe–Ti oxides in layered mafic intrusions, we investigate Mg isotopic compositions of magnetite, coupled with its chemical data and whole-rock maj
Autor:
Qing-Lin Liang, Xie-Yan Song, Richard Wirth, Lie-Meng Chen, Song-Yue Yu, Nadezhda A. Krivolutskaya, Zhi-Hui Dai
Publikováno v:
Geochimica et Cosmochimica Acta
In magmatic Nickel-Copper-Platinum-group elements (Ni-Cu-PGE) sulfide deposits, PGE occur as solid solution in base metal sulfides (BMS) or occur as platinum-group minerals (PGM). In different deposits, such as the world-class deposits at Jinchuan an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0c90f90a7e0b9dd57f0b82bee2b6101a
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5010424
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5010424
Publikováno v:
American Mineralogist. 105:479-497
Chromite is one of the earliest crystallized minerals from mafic melts and has been used as an important “petrogenetic indicator.” Its composition may be modified by interaction with intercumulate melt and adjacent minerals. Thus, chromite in maf
Publikováno v:
Ore Geology Reviews. 144:104837