Vv. Shcherbakova et al., ON THE EFFECT OF LOW-TEMPERATURE DEMAGNETIZATION ON TRMS AND PTRMS, Geophysical journal international, 127(2), 1996, pp. 379-386
Low-temperature demagnetization (LTD) experiments with TRMs and pTRMs
using liquid nitrogen were carried out on samples with different (MD a
nd PSD) domain structures to infer and to compare the type of domain s
tructure of samples before and after LTD judged by the thermomagnetic
criterion. This is based on testing materials against Thellier's law o
f independence of pTRMs. The results demonstrate good agreement betwee
n the commonly used criteria for differentiating domain structure, suc
h as Q(rt), H-cr/H-c and I-rs/I-s factors, and more sophisticated ones
, such as the thermomagnetic criterion and LTD treatment. It is notewo
rthy that there is no observable tendency of MD or PSD samples to disp
lay SD-type pTRM =f(T) curves after LTD treatment. Hence our experimen
ts failed to detect a quasi-SD component of remanence acquiring TRM by
thermofluctuations in MD or PSD grains in the manner of Verhoogen (19
59) and Stacey & Banerjee (1974) hypotheses