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Geofluids
Volume 2017 (2017), Article ID 4094582, 19 pages
https://doi.org/10.1155/2017/4094582
Research Article

Fluid Inclusion and Oxygen Isotope Constraints on the Origin and Hydrothermal Evolution of the Haisugou Porphyry Mo Deposit in the Northern Xilamulun District, NE China

1State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2Key Laboratory of Orogenic Belt and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China

Correspondence should be addressed to Qihai Shu

Received 14 July 2017; Accepted 2 October 2017; Published 1 November 2017

Academic Editor: Bin Chen

Copyright © 2017 Qihai Shu and Yong Lai. 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

Qihai Shu and Yong Lai, “Fluid Inclusion and Oxygen Isotope Constraints on the Origin and Hydrothermal Evolution of the Haisugou Porphyry Mo Deposit in the Northern Xilamulun District, NE China,” Geofluids, vol. 2017, Article ID 4094582, 19 pages, 2017. doi:10.1155/2017/4094582