Detailed alternating field (AF) demagnetization of Natural Remanent Magnetization (NRM) was conducted on u-channel samples of sediment core PS72/396-5, complemented by Anhysteretic Remanent Magnetization (ARM) and Isothermal Remanent Magnetization (IRM) acquisition measurements and subsequent demagnetization. AF demagnetization data of NRM were analyzed using anchored Principal Component Analysis (PCA) to obtain the Characteristic Remanent Magnetization (ChRM). A number of parameters, i.e. median destructive fields (MDF of NRM, ARM, and IRM), pseudo S-ratio, ratio of ARM to IRM Intensities, both demagnetized at an alternating field of 100 mT, was calculated
Rock magnetic parameters for the sediment core from anhysteretic remanent magnetization, isothermal ...
Natural remanent magnetization and demagnetization data of SWERUS-C3-L2-13-PC. Dataset also includes...
Abstract Previous studies have compiled relative paleointensity data for the last 2–3 Ma from indivi...
Detailed alternating field (AF) demagnetization of Natural Remanent Magnetization (NRM) were conduct...
Measurements of alternating field demagnetization of natural remanent magnetization (NRM). Measureme...
Calculations of Characteristic remanent magnetization and median destructive field of NRM. A vector ...
Paleomagnetic and rockmagnetic studies were carried out in order to investigate the characteristics ...
AF demagnetization characteristics and isothermal remanent magnetization (IRM) acquisition of a vari...
Measurements of acquisition of isothermal remanent magnetization (IRM) and its subsequent alternatin...
Measurements of acquisition of anhysteretic remanent magnetization (ARM) and its subsequent alternat...
Observations of the Earth's magnetic field discovered dramatic changes of its intensity. In the last...
[1] One necessary condition for successful determination of relative paleomagnetic field intensity u...
To identify remagnetization is essential for palaeomagnetic studies and their geodynamic implication...
Rock magnetic parameters for the sediment core from anhysteretic remanent magnetization, isothermal ...
Rock magnetic parameters for the sediment core from anhysteretic remanent magnetization, isothermal ...
Rock magnetic parameters for the sediment core from anhysteretic remanent magnetization, isothermal ...
Natural remanent magnetization and demagnetization data of SWERUS-C3-L2-13-PC. Dataset also includes...
Abstract Previous studies have compiled relative paleointensity data for the last 2–3 Ma from indivi...
Detailed alternating field (AF) demagnetization of Natural Remanent Magnetization (NRM) were conduct...
Measurements of alternating field demagnetization of natural remanent magnetization (NRM). Measureme...
Calculations of Characteristic remanent magnetization and median destructive field of NRM. A vector ...
Paleomagnetic and rockmagnetic studies were carried out in order to investigate the characteristics ...
AF demagnetization characteristics and isothermal remanent magnetization (IRM) acquisition of a vari...
Measurements of acquisition of isothermal remanent magnetization (IRM) and its subsequent alternatin...
Measurements of acquisition of anhysteretic remanent magnetization (ARM) and its subsequent alternat...
Observations of the Earth's magnetic field discovered dramatic changes of its intensity. In the last...
[1] One necessary condition for successful determination of relative paleomagnetic field intensity u...
To identify remagnetization is essential for palaeomagnetic studies and their geodynamic implication...
Rock magnetic parameters for the sediment core from anhysteretic remanent magnetization, isothermal ...
Rock magnetic parameters for the sediment core from anhysteretic remanent magnetization, isothermal ...
Rock magnetic parameters for the sediment core from anhysteretic remanent magnetization, isothermal ...
Natural remanent magnetization and demagnetization data of SWERUS-C3-L2-13-PC. Dataset also includes...
Abstract Previous studies have compiled relative paleointensity data for the last 2–3 Ma from indivi...