It is confirmed by new magnetization measurements that a magnetic transition occurs sharply at 30 K in the monoclinic pyrrhotite Fe7S8. Though its nature is not yet fully understood, this transition shows some similarities with the Verwey transition and can provide a powerful tool for the identification of pyrrhotite in rocks
© 2016 Elsevier B.V..Here we present a comprehensive magnetic characterization of synthesized non-id...
Iron mono-sulphides, or pyrrhotites, are minerals present in the Earth's crust and mantle as well as...
The monosulfides of the pyrrhotite omission series (Fe1xS; 0 < x 0:125) are important remanence carr...
A characteristic magnetic transition at 30-34 K is shown to provide a powerful tool for the identifi...
Use of low temperature (LT) magnetic transitions to identify magnetic minerals that carry a remanen...
The low‐temperature magnetic properties of the many pyrrhotite varieties have not been studied exten...
International audiencePyrrhotite is a common ferrimagnetic mineral in terrestrial rocks and has been...
Ferrimagnetic, monoclinic 4C pyrrhotite (Fe7S8) is the only iron sulphide with high relevance for pa...
Pyrrhotite, Fe7S8, is a commonly occurring carrier of magnetic remanence and has a low temperature t...
Monoclinic 4C pyrrhotite (Fe7S8) is ferrimagnetic due to an ordered defect structure with alternatin...
Monoclinic pyrrhotite (Fe7S8) is widely claimed to carry magnetizations acquired during early diagen...
Abstract: Pyrrhotite, Fe7S8, is a commonly occurring carrier of magnetic remanence and has a low tem...
We report the discovery of a low temperature spin-flop transition in 5C pyrrhotite at ~155 K that is...
The magnetic behaviour of magnetite at low temperatures is dominated by its transformation to a mono...
The sulfur-rich limit of hexagonal pyrrhotite below 290 ø C is 47.45 atomic percent iron and is inde...
© 2016 Elsevier B.V..Here we present a comprehensive magnetic characterization of synthesized non-id...
Iron mono-sulphides, or pyrrhotites, are minerals present in the Earth's crust and mantle as well as...
The monosulfides of the pyrrhotite omission series (Fe1xS; 0 < x 0:125) are important remanence carr...
A characteristic magnetic transition at 30-34 K is shown to provide a powerful tool for the identifi...
Use of low temperature (LT) magnetic transitions to identify magnetic minerals that carry a remanen...
The low‐temperature magnetic properties of the many pyrrhotite varieties have not been studied exten...
International audiencePyrrhotite is a common ferrimagnetic mineral in terrestrial rocks and has been...
Ferrimagnetic, monoclinic 4C pyrrhotite (Fe7S8) is the only iron sulphide with high relevance for pa...
Pyrrhotite, Fe7S8, is a commonly occurring carrier of magnetic remanence and has a low temperature t...
Monoclinic 4C pyrrhotite (Fe7S8) is ferrimagnetic due to an ordered defect structure with alternatin...
Monoclinic pyrrhotite (Fe7S8) is widely claimed to carry magnetizations acquired during early diagen...
Abstract: Pyrrhotite, Fe7S8, is a commonly occurring carrier of magnetic remanence and has a low tem...
We report the discovery of a low temperature spin-flop transition in 5C pyrrhotite at ~155 K that is...
The magnetic behaviour of magnetite at low temperatures is dominated by its transformation to a mono...
The sulfur-rich limit of hexagonal pyrrhotite below 290 ø C is 47.45 atomic percent iron and is inde...
© 2016 Elsevier B.V..Here we present a comprehensive magnetic characterization of synthesized non-id...
Iron mono-sulphides, or pyrrhotites, are minerals present in the Earth's crust and mantle as well as...
The monosulfides of the pyrrhotite omission series (Fe1xS; 0 < x 0:125) are important remanence carr...
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