Integrated O–Sr–Nd isotope constraints on the evolution of four important Fe–Ti oxide ore-bearing mafic–ultramafic intrusions in the Emeishan large igneous province, SW China

2015/02/26 by Song-Yue Yu, Song‐Yue Yu, Xie‐Yan Song +6 · 32 citations
Earth and Planetary Sciences · #Anorthosite #Basalt #Chromite #Chromitite #Geochemistry #Geological and Geochemical Analysis #Geology #High-pressure geophysics and materials #Igneous rock #Large igneous province #Layered intrusion #Mafic #Magma #Magmatism #Metamorphism #Paleontology #Plagioclase #Ultramafic rock #earthquake and tectonic studies

paper · doi:10.1016/j.chemgeo.2015.02.020

published in Chemical Geology 401, 28-42 (Elsevier BV)

openalex publication_date 2015/02/26 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/28

Citations

• Zircon U–Pb and Hf isotope constraints on crustal melting associated with the Emeishan mantle plume
• Distinct mantle sources of low-Ti and high-Ti basalts from the western Emeishan large igneous province, SW China: implications for plume–lithosphere interaction
• Chemical mass transfer in magmatic processes IV. A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures
• The Lu–Hf and Sm–Nd isotopic composition of CHUR: Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets
• A temporal link between the Emeishan large igneous province (SW China) and the end-Guadalupian mass extinction
• Petrogenesis of the Pt–Pd mineralized Jinbaoshan ultramafic intrusion in the Permian Emeishan Large Igneous Province, SW China
• Origin of Fe-Ti Oxide Ores in Mafic Intrusions: Evidence from the Panzhihua Intrusion, SW China
• Geochemistry, Petrogenesis and Metallogenesis of the Panzhihua Gabbroic Layered Intrusion and Associated Fe–Ti–V Oxide Deposits, Sichuan Province, SW China

Cited by

• Multi-component crustal recycling recorded by LiMg isotopes in Emeishan mafic–ultramafic layered intrusions with implications for Fe–Ti–V metallogeny