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On the Reliability of Absolute Palaeointensity Determinations on Vasaltic Rocks Bearing a Thermochemical Remanence of thermochemical remanent magnetization (TCRM) on basaltic rocks from the volcanic island of São Tomé (Gulf

Experimental modeling of the chemical remanent magnetization and Thellier procedure on titanomagnetite-bearing basalts and partial thermal remanent magnetizations (or their combination), which are imparted at the initial stage

Experimental modeling of the chemical remanent magnetization and Thellier procedure on titanomagnetite-bearing basalts and partial thermal remanent magnetizations (or their combination), which are imparted at the initial stage

Experimental and numerical simulation of the acquisition of chemical remanent magnetization and the Thellier procedure determination on the samples which contain chemical remanent magnetization (CRM) created by thermal annealing

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

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