Widespread occurrence of silicate‐hosted magnetic mineral inclusions in marine sediments and their contribution to paleomagnetic recording

Magnetic mineral inclusions occur commonly within other larger mineral phases in igneous rocks and have been demonstrated to preserve important paleomagnetic signals. While the usefulness of magnetic inclusions in igneous rocks has been explored extensively, their presence in sediments has only been...

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Veröffentlicht in:	Journal of geophysical research. Solid earth 2016-12, Vol.121 (12), p.8415-8431
Hauptverfasser:	Chang, Liao, Roberts, Andrew P., Heslop, David, Hayashida, Akira, Li, Jinhua, Zhao, Xiang, Tian, Wei, Huang, Qinghua
Format:	Artikel
Sprache:	eng
Schlagworte:	Chemical composition Clay Clay minerals Computer simulation Deposition detrital remanent magnetization Diagenesis Forces (mechanics) Geomagnetism Geophysics Grain size Gravitation Gravity Hydrodynamics Igneous rocks Inclusions Iron Iron oxides Magnetic methods magnetic mineral inclusions Magnetic studies Magnetism Magnetization Marine sediments Microstructure Mineral inclusions Minerals Modelling Nanostructure Oxides Paleomagnetism Particle physics Phases Preservation Protection Quartz Recording Remanent magnetization Rock Sediment Sediments Silicate minerals Silicates Simulation Sulfate reduction TEM Transmission electron microscopy
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