Distinction between S-type and peraluminous I-type granites: Zircon versus whole-rock geochemistry

2016/04/29 by Peng Gao, Yong-Fei Zheng, Yong‐Fei Zheng +2
Earth and Planetary Sciences · #Geological and Geochemical Analysis #High-pressure geophysics and materials #earthquake and tectonic studies

paper · doi:10.1016/j.lithos.2016.04.019

Citations

• Metasedimentary melting in the formation of charnockite: Petrological and zircon U-Pb-Hf-O isotope evidence from the Darongshan S-type granitic complex in southern China
• Zircon megacrysts from kimberlite: oxygen isotope variability among mantle melts
• Aluminium saturation in I- and S-type granites and the characterization of fractionated haplogranites
• Magma to mud to magma: Rapid crustal recycling by Permian granite magmatism near the eastern Gondwana margin
• Continental and Oceanic Crust Recycling-induced Melt-Peridotite Interactions in the Trans-North China Orogen: U-Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths
• What controls chemical variation in granitic magmas?
• Plešovice zircon — A new natural reference material for U–Pb and Hf isotopic microanalysis