Shock experiments up to 30 GPa and their consequences on microstructures and magnetic properties in pyrrhotite-Reference-Cited by-同舟云学术

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Shock experiments up to 30 GPa and their consequences on microstructures and magnetic properties in pyrrhotite

Published:2013-01 Issue:1 Volume:14 Page:64-85
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Mang Christoph¹,Kontny Agnes¹,Fritz Jörg²,Schneider Reinhard³

Affiliation:

1. Institut für Angewandte Geowissenschaften, Karlsruher Institut für Technologie; Adenauerring 20, Geb. 50.40 D-76131 Karlsruhe Germany

2. Museum für Naturkunde; Leibniz-Institut an der Humboldt Universität zu Berlin; Berlin Germany

3. Laboratorium für Elektronenmikroskopie, Karlsruher Institut für Technologie; Karlsruhe Germany

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference89 articles.

1. Equations of State of Iron Sulfide and Constraints on the Sulfur Content of the Earth;Ahrens;J. Geophys. Res.,1979

2. Shock melting and vaporization of lunar rocks and minerals;Ahrens;Earth, Moon Planets,1972

3. Shock Wave Experiments on Iron Sulfide and Sulfur in Planetary Cores;Anderson;Lun. Planet. Sci.,1986

4. Influence of nonstoichiometry on the Verwey transition;Aragón;Phys. Rev. B,1985

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

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