 | Wang, Hui, Feng, Chengyou, Li, Rongxi, Li, Daxin (2018) Geological characteristics, metallogenesis, and tectonic setting of porphyry-skarn Cu deposits in East Kunlun Orogen. Geological Journal, 53. 58-76 doi:10.1002/gj.3130 | Journal (article/letter/editorial) | | ARTICLE Geological characteristics, metallogenesis, and tectonic setting of porphyry–skarn Cu deposits in...of Earth Science and Resources, Chang'an University, Xi'an, Shaanxi Province, China 2 Key Laboratory...Resources and Geological Engineering, Ministry of Education, Xi'an, Shaanxi Province, China 3 Institute...Geological Sciences, Beijing, China Correspondence Hui Wang, School of Earth Science and Resources, Chang'an University...Xi'an, China. Email: wang_hui2007@qq.com Funding information Geological Survey Program from the China Geological |  | | Book | | Mountains, Qinghai Province Springer Theses Recognizing Outstanding Ph.D. Research Aims and Scope The...theses from around the world and across the physical sciences. Nominated and endorsed by two recognized...volume has been selected for its scientific excellence and the high impact of its contents for the pertinent...both for newcomers to the research fields described, and for other scientists seeking detailed background...accepted into the series by invited nomination only and must fulfill all of the following criteria • They |  | Yu, M., Feng, C. -Y., Zhu, Y. -F., Mao, J. -W., Zhao, Y. -M., Li, D. -X. (2017) Multistage amphiboles from the Galinge iron skarn deposit in Qiman Tagh, western China: evidence of igneous rocks replacement. Mineralogy and Petrology, 111 (1) 81-97 doi:10.1007/s00710-016-0459-x | Journal (article/letter/editorial) | | Galinge iron skarn deposit in Qiman Tagh, western China: evidence of igneous rocks replacement M. Yu 1,2...deposit in the Qiman Tagh metallogenic belt (western China), were formed by multistage fluid-rock interactions...hornblende (FE); Amp-II: Deep bluish-green magnesian-hastingsite (MH); Amp-III: Light greenish-beige ferro-actinolite...preserves the primary igneous amphibole composition, and was subsequently replaced by Amp-II. The amphibole...176 − 0.582 wt.%) to the MH (0.894 − 3.161 wt.%), and abruptly drops in the FA (0.017 − 0.039 wt.%). The |
|
