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Pre- and syn-eruptive conditions inferred from the magnetic petrology of Fe-Ti oxides from three historical eruptions of Unzen Volcano, Japan
Takeshi Saito
*
,
Naoto Ishikawa
*
Corresponding author for this work
Earth System Science
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Article
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peer-review
6
Scopus citations
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Keyphrases
Japan
100%
Fe-Ti Oxides
100%
Pre-eruptive
100%
Magnetic Petrology
100%
Unzen Volcano
100%
Magma Chamber
100%
Syn-eruptive
100%
Historical Eruptions
100%
Lava
80%
Lava Flow
80%
Magma
60%
Phenocrysts
40%
Mafic Magma
40%
Low Temperature
20%
Ilmenite
20%
High Temperature
20%
Lava Dome
20%
Oxygen Fugacity
20%
Low Viscosity
20%
Viscosity
20%
Ti Content
20%
High Viscosity
20%
Nickel Oxide
20%
Magma Mixing
20%
High Curie Temperature
20%
Microlite
20%
Earth and Planetary Sciences
Japan
100%
Magma
100%
Petrography
100%
Magma Chamber
83%
Lava Flow
66%
Phenocryst
33%
Ilmenite
16%
Lava Dome
16%
Fugacity
16%
Nickel Oxide
16%
Curie Temperature
16%