Petrogenetic implications of mineral chemical data for the Permian Baima igneous complex, SW China

2012/07/04 by J. Gregory Shellnutt, Kwan-Nang Pang, Kwan‐Nang Pang
Computer Science · Earth and Planetary Sciences · #Geochemistry and Geologic Mapping #Geological and Geochemical Analysis #High-pressure geophysics and materials

paper · doi:10.1007/s00710-012-0217-7

openalex publication_date 2012/07/04 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/29

Citations

• Mineral compositional constraints on petrogenesis and oxide ore genesis of the late Permian Panzhihua layered gabbroic intrusion, SW China
• 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
• Permian peralkaline, peraluminous and metaluminous A-type granites in the Panxi district, SW China: Their relationship to the Emeishan mantle plume
• Two magma series and associated ore deposit types in the Permian Emeishan large igneous province, SW China
• Petrologic and geochemical constraints on the petrogenesis of Permian–Triassic Emeishan flood basalts in southwestern China
• 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
• A temporal link between the Emeishan large igneous province (SW China) and the end-Guadalupian mass extinction
• Olivine-liquid equilibrium
• Abundant Fe–Ti oxide inclusions in olivine from the Panzhihua and Hongge layered intrusions, SW China: evidence for early saturation of Fe–Ti oxides in ferrobasaltic magma
• Origin of Fe-Ti Oxide Ores in Mafic Intrusions: Evidence from the Panzhihua Intrusion, SW China