The low‐temperature magnetic properties of the many pyrrhotite varieties have not been
studied extensively. Monoclinic pyrrhotite (Fe7S8) goes through the Besnus transition at~ 30 …

SUMMARY The Holy Cross Mountains (HCM) in Poland, is an isolated natural outcrop of
Palaeozoic rocks located within the Trans-European Suture Zone, a tectonic collage of …

Seismic slip zones convey important information on earthquake energy dissipation and
rupture processes. However, geological records of earthquakes along exhumed faults …

A group-theoretical framework to describe vacancy ordering and magnetism in the Fe1− xS
system is developed. This framework is used to determine the sequence of crystal structures …

Ferrimagnetic, monoclinic 4C pyrrhotite (Fe7S8) is the only iron sulphide with high
relevance for palaeomagnetism and rock magnetism that can be identified in rock materials …

Abstract Pyrrhotite, Fe 7 S 8, is a commonly occurring carrier of magnetic remanence and
has a low temperature transition, the Besnus transition, involving a change in spin state …

Structural defects on an atomic level can crucially impact the magnetic properties of a
material. We study this phenomenon by means of magnetometry and powder neutron …

Abstract Pyrrhotite, Fe7S8, is a common sulfide mineral in the Earth's crust and mantle, as
well as in a range of meteorites and is of interest to a wide variety of disciplines including …

The discontinuous change in magnetic properties at a temperature of about 32 K, denoted
as the Besnus transition, is a diagnostic feature for detecting 4C pyrrhotite in geological …

Non-stoichiometric monoclinic 4C pyrrhotite (Fe 7 S 8), a ferrimagnetic monosulfide that has
been intensively used as a remanence carrier to infer the magnetization of the Earth's crust …