Oriented Magnetite Inclusions in Plagioclase: Implications for the Anisotropy of Magnetic Remanence-Reference-Cited by-同舟云学术

Oriented Magnetite Inclusions in Plagioclase: Implications for the Anisotropy of Magnetic Remanence

Published:2022-02 Issue:2 Volume:23 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Ageeva O.¹²^ORCID,Habler G.¹^ORCID,Gilder S. A.³^ORCID,Schuster R.⁴^ORCID,Pertsev A.²^ORCID,Pilipenko O.⁵^ORCID,Bian G.¹^ORCID,Abart R.¹^ORCID

Affiliation:

1. Department of Lithospheric Research University of Vienna Vienna Austria

2. Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry Russian Academy of Sciences Moscow Russia

3. Department of Earth and Environmental Sciences Ludwig Maximilians University Munich Germany

4. Christian Doppler Laboratory for Interfaces and Precipitation Engineering (CDL‐IPE) Institute of Materials Science and Technology, TU Wien Vienna Austria

5. Schmidt Institute of Physics of the Earth Russian Academy of Sciences Moscow Russia

Funder

Austrian Science Fund

Russian Foundation for Basic Research

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC010272

Reference71 articles.

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2. Fe-Ti oxide micro-inclusions in clinopyroxene of oceanic gabbro: Phase content, orientation relations and petrogenetic implication

3. Plagioclase hosted Fe-Ti-oxide micro-inclusions in an oceanic gabbro-plagiogranite association from the Mid Atlantic ridge at 13 34' N

4. Microstructure evolution of plagioclase-hosted Fe-Ti-oxide microinclusions in oceanic gabbro

5. Magnetic properties of FeO‐Fe2O3‐TiO2 system as a basis of rock magnetism;Akimoto S.;Journal of the Physical Society of Japan,1962

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3. Oriented secondary magnetite micro-inclusions in plagioclase from oceanic gabbro;American Mineralogist;2023-09-01

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