Thermoremanence acquisition and demagnetization for titanomagnetite under lithospheric pressures of the geological sources of magnetic anomalies. We present thermal
remanent magnetization (TRM) acquisition
Origin of false components of NRM during conventional stepwise thermal demagnetization to conventional stepwise thermal demagnetization at 250-450 °C display mid-temperature
remanence (MTC) directed
Titanomagnetites with Magnetite–Ulvospinel breakdown structures. Coercive properties: modeling and experiment and the state of
remanent saturation magnetization. A distinctive feature of these models is the calculation
Thermoremanence acquisition and demagnetization for titanomagnetite under lithospheric pressures of the geological sources of magnetic anomalies. We present thermal
remanent magnetization (TRM) acquisition
Titanomagnetites with Magnetite–Ulvospinel breakdown structures. Coercive properties: modeling and experiment and the state of
remanent saturation magnetization. A distinctive feature of these models is the calculation
Origin of false components of NRM during conventional stepwise thermal demagnetization to conventional stepwise thermal demagnetization at 250-450 °C display mid-temperature
remanence (MTC) directed