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Geofluids
Volume 2017, Article ID 3107280, 21 pages
https://doi.org/10.1155/2017/3107280
Research Article

Origin and Evolution of the Ore-Forming Fluids in the Liyuan Gold Deposit, Central North China Craton: Constraints from Fluid Inclusions and H-O-C Isotopic Compositions

1State Key Laboratory of Geological Processes and Mineral Resources, Faculty of Earth Resources, Collaborative Innovation Center for Exploration of Strategic Mineral Resources, China University of Geosciences, Wuhan 430074, China
2School of Earth Sciences, East China University of Technology, Nanchang 330013, China
3State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China

Correspondence should be addressed to Shao-Yong Jiang; nc.ude.guc@gnaijyhs

Received 28 January 2017; Accepted 6 June 2017; Published 7 August 2017

Academic Editor: Paolo Fulignati

Copyright © 2017 Ying Ma et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

How to Cite this Article

Ying Ma, Suo-Fei Xiong, Hua-Liang Li, and Shao-Yong Jiang, “Origin and Evolution of the Ore-Forming Fluids in the Liyuan Gold Deposit, Central North China Craton: Constraints from Fluid Inclusions and H-O-C Isotopic Compositions,” Geofluids, vol. 2017, Article ID 3107280, 21 pages, 2017. https://doi.org/10.1155/2017/3107280.