The Low‐Temperature Besnus Magnetic Transition: Signals Due to Monoclinic and Hexagonal Pyrrhotite-Reference-Cited by-同舟云学术

The Low‐Temperature Besnus Magnetic Transition: Signals Due to Monoclinic and Hexagonal Pyrrhotite

Published:2018-09 Issue:9 Volume:19 Page:3364-3375
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Horng Chorng‐Shern¹^ORCID,Roberts Andrew P.²^ORCID

Affiliation:

1. Institute of Earth Sciences Academia Sinica Nangang, Taipei Taiwan

2. Research School of Earth Sciences Australian National University Canberra ACT Australia

Funder

Central Geological Survey, Ministry of Economic Affairs

Australian Research Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2017GC007394

Reference59 articles.

1. Mixtures of hexagonal and monoclinic pyrrhotite and the measurement of the metal content of pyrrhotite by X‐ray diffraction;Arnold R. G.;American Mineralogist,1966

2. Nickel distribution in hexagonal and monoclinic pyrrhotite;Batt A. P.;Canadian Mineralogist,1972

3. New observations on natural pyrrhotites: Magnetic transition in hexagonal pyrrhotite;Bennett C. E. G.;American Mineralogist,1981

4. Besnus M. J. &Meyer A. J.(1964).Nouvelles données expérimentales sur le magnétisme de la pyrrhotine naturelle. Paper Presented at Proceedings of the International Conference on Magnetism Nottingham England 507–511.

5. Low-temperature magnetic properties of greigite (Fe3S4)

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