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

2008/02/26 by Kwan-Nang Pang, Kwan‐Nang Pang, Chusi Li +3 · 6 citations
Earth and Planetary Sciences · Biochemistry, Genetics and Molecular Biology · #Geological and Geochemical Analysis #Geomagnetism and Paleomagnetism Studies #High-pressure geophysics and materials

paper · doi:10.1007/s00410-008-0287-z

Citations

• 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

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• Apatite-hosted melt inclusions from the Panzhihua gabbroic-layered intrusion associated with a giant Fe–Ti oxide deposit in SW China: insights for magma unmixing within a crystal mush
• Composition of the Chilled Marginal Rocks of the Panzhihua Layered Intrusion, Emeishan Large Igneous Province, SW China: Implications for Parental Magma Compositions, Sulfide Saturation History and Fe–Ti Oxide Mineralization
• Mineral compositional constraints on petrogenesis and oxide ore genesis of the late Permian Panzhihua layered gabbroic intrusion, SW China
• Timing of Ti-magnetite crystallisation and silicate disequilibrium in the Panzhihua mafic layered intrusion: Implications for ore-forming processes
• Open magma chamber processes in the formation of the Permian Baima mafic–ultramafic layered intrusion, SW China
• Multi-component crustal recycling recorded by LiMg isotopes in Emeishan mafic–ultramafic layered intrusions with implications for Fe–Ti–V metallogeny