Fluid Evolution and Scheelite Precipitation Mechanism of the Large-Scale Shangfang Quartz-Vein-Type Tungsten Deposit, South China: Constraints from Rare Earth Element (REE) Behaviour during Fluid/Rock Interaction
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s12583-020-1283-0.pdf
Reference69 articles.
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2. Brugger, J., Lahaye, Y., Costa, S., et al., 2000b. Inhomogeneous Distribution of REE in Scheelite and Dynamics of Archaean Hydrothermal Systems (Mt. Charlotte and Drysdale Gold Deposits, Western Australia). Contributions to Mineralogy and Petrology, 139(3): 251–264. https://doi.org/10.1007/s004100000135
3. Burt, D. M., 1989. Compositional And Phase-Relations Among Rare-Earth Element Minerals. Reviews in Mineralogy, 21: 259–307
4. Charvet, J., 2013. The Neoproterozoic-Early Paleozoic Tectonic Evolution of the South China Block: An Overview. Journal of Asian Earth Sciences, 74: 198–209. https://doi.org/10.1016/j.jseaes.2013.02.015
5. Chen, C., Lü, X. B., Wu, C. M., et al., 2018. Origin and Geodynamic Implications of Concealed Granite in Shadong Tungsten Deposit, Xinjiang, China: Zircon U-Pb Chronology, Geochemistry, and Sr-Nd-Hf Isotope Constraint. Journal of Earth Science, 29(1): 114–129. https://doi.org/10.1007/s12583-017-0808-7
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