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 · 149 citations
Earth and Planetary Sciences · #Basalt #Biotite #Continental crust #Crust #Geochemistry #Geological and Geochemical Analysis #Geology #High-pressure geophysics and materials #Magmatism #Paleontology #Paleozoic #Partial melting #Petrogenesis #Petrology #Quartz #Zircon #earthquake and tectonic studies

paper · doi:10.1016/j.lithos.2016.04.019

published in Lithos 258-259, 77-91 (Elsevier BV)

openalex publication_date 2016/04/29 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/28

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