Although most paleomagnetic and environmental magnetic papers incorporate a Day plot of
the hysteresis parameters Mrs/Ms versus Hcr/Hc, a comprehensive theory covering …

Hysteresis measurements have become an important part of characterizing magnetic
behavior of rocks in paleomagnetic studies. Theoretical interpretation is often difficult owing …

We hypothesize that the rapid onset of the carbon isotope excursion (CIE) at the
Paleocene/Eocene boundary (∼ 55 Ma) may have resulted from the accretion of a …

Plots of the first‐order reversal curve (FORC) function are used to characterize ferromagnetic
particles in rocks. The function is based on classical Preisach theory, which represents …

Laboratory-induced remanent magnetization of polar ice constitutes a measurement of the
magnetization carried by the ferromagnetic dust particles in the ice. This non-destructive …

From experiments it is known that magnetostatic interactions between grains strongly affect
the magnetic behavior of samples. However, because of the difficulty in predicting the …

The standard paradigm that the Paleocene/Eocene thermal maximum (PETM) represents a
threshold event intrinsic to Earth's climate and connected in some way with long-term …

First-order reversal curve (FORC) diagrams have been experimentally shown to be a better
way of discriminating domain states in a sample compared to the straightforward use of …

Paleocene carbonates from the Gamba area of South Tibet provide the largest
paleomagnetic dataset for constraining the paleogeography of the India-Asia collision in the …

Synthetic hysteresis loops were generated by numerically solving the classical Stoner‐
Wohlfarth model and a thermally activated Stoner‐Wohlfarth model for a set of randomly …