The anhysteretic remanent magnetization (ARM) is an important magnetic parameter for
quantifying the concentration of “fine”, mostly sub‐micron ferrimagnetic particles in rocks and …

Understanding magnetostatic interactions in sediments is important for paleomagnetism and
rock magnetism. Magnetostatic interactions are known to affect significantly the efficiency of …

Magnetic parameters are used extensively to interpret magnetic mineral assemblage
variations in environmental studies. Conventional room temperature measurements of bulk …

Marine sediments can preserve continuous paleomagnetic intensity records. Different
magnetic minerals may acquire remanent magnetizations differently, so that compositional …

Widespread geological preservation of biogenic magnetite makes it important to assess how
such particles contribute to sedimentary paleomagnetic signals. We studied a sediment core …

An environmental magnetic study was conducted to investigate temporal variations of the
sources of magnetic minerals in the Pacific Ocean using sediment cores of Pleistocene age …

Geomagnetic field intensity records from marine sediments have contributed to improved
understanding of variations in the Earth's magnetic field, and have helped to establish age …

Marine sediments record direction and intensity of the Earth's magnetic field by the
alignment of magnetic particles during deposition. For determining relative paleointensity …

Sedimentary relative paleointensity (RPI) records are often carried by complex magnetic
mineral mixtures, including detrital and biogenic magnetic minerals. Recent studies have …

We present a general theory for the acquisition of natural remanent magnetizations (NRM) in
sediment under the influence of (a) magnetic torques,(b) randomizing torques, and (c) …