Origin of oscillatory zoned garnets from the Xieertala Fe–Zn skarn deposit, northern China: In situ LA–ICP-MS evidence

2014/01/03 by De-Gao Zhai, Degao Zhai, Jiajun Liu +10 · 3 citations
Earth and Planetary Sciences · #Geological and Geochemical Analysis #Geochemistry and Elemental Analysis #Geology and Paleoclimatology Research

paper · doi:10.1016/j.lithos.2013.12.017

Citations

• REE in skarn systems: A LA-ICP-MS study of garnets from the Crown Jewel gold deposit
• The composition of the Earth
• Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium
• REE controls in ultramafic hosted MOR hydrothermal systems: An experimental study at elevated temperature and pressure
• The Rare Earth Elements and Uranium in Garnets from the Beinn an Dubhaich Aureole, Skye, Scotland, UK: Constraints on Processes in a Dynamic Hydrothermal System
• On the formation and structure of rare-earth element complexes in aqueous solutions under hydrothermal conditions with new data on gadolinium aqua and chloro complexes
• Significance of oscillatory and bell-shaped growth zoning in hydrothermal garnet: Evidence from the Navachab gold deposit, Namibia
• Europium redox equilibria in aqueous solution

Cited by

• The formation and trace elements of garnet in the skarn zone from the Xinqiao Cu-S-Fe-Au deposit, Tongling ore district, Anhui Province, Eastern China
• Skarn formation and trace elements in garnet and associated minerals from Zhibula copper deposit, Gangdese Belt, southern Tibet
• Textural and geochemical characteristics of garnet from the Luoyang Fe skarn deposit, eastern China: implications for ore-forming fluid evolution and mineralization conditions