Low-temperature magnetic transition in troilite: A simple marker for highly stoichiometric FeS systems

Author:

Cuda J.1,Kohout T.23,Tucek J.1,Haloda J.4,Filip J.1,Prucek R.1,Zboril R.1

Affiliation:

1. Regional Centre of Advanced Technologies and Materials, Departments of Physical Chemistry and Experimental Physics; Palacky University; Olomouc Czech Republic

2. Department of Physics; University of Helsinki; Helsinki Finland

3. Institute of Geology; Academy of Sciences of the Czech Republic v.v i.; Prague Czech Republic

4. Czech Geological Survey; Prague Czech Republic

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference24 articles.

1. Equilibrium relations between pyrrhotite and pyrite from 325° to 743°C;Arnold;Econ. Geol.,1962

2. Measurement of the metal content of naturally occurring, metal-deficient, hexagonal pyrrhotite by an x-ray spacing method;Arnold;Am. Mineral.,1962

3. Rock Magnetism

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