Izumi Mashino

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Science, Ph.D, Tohoku University

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7 Article
1 Chapter

Acoustic Wave Velocities of Ferrous-Bearing MgSiO₃ Glass up to 158 GPa With Implications for Dense Silicate Melts at the Base of the Earth's Mantle
Mashino, I., Murakami, M., Kitao, S., Mitsui, T., Masuda, R. & Seto, M., Oct 16 2022, In: Geophysical Research Letters. 49, 19, e2022GL098279.
Research output: Contribution to journal › Article › peer-review
1 Citation (Scopus)
A cylindrical SiC heater for an externally heated diamond anvil cell to 1500 K
Okuda, Y., Kimura, S., Ohta, K., Park, Y., Wakamatsu, T., Mashino, I. & Hirose, K., Jan 1 2021, In: Review of Scientific Instruments. 92, 1, 015119.
Research output: Contribution to journal › Article › peer-review

Open Access
3 Citations (Scopus)
Experimental evidence for silica-enriched Earth’s lower mantle with ferrous iron dominant bridgmanite
Mashino, I., Murakami, M., Miyajima, N. & Petitgirard, S., Nov 10 2020, In: Proceedings of the National Academy of Sciences of the United States of America. 117, 45, p. 27899-27905 7 p.
Research output: Contribution to journal › Article › peer-review
17 Citations (Scopus)
Melting experiments on the Fe–C binary system up to 255 GPa: Constraints on the carbon content in the Earth's core
Mashino, I., Miozzi, F., Hirose, K., Morard, G. & Sinmyo, R., Jun 1 2019, In: Earth and Planetary Science Letters. 515, p. 135-144 10 p.
Research output: Contribution to journal › Article › peer-review
43 Citations (Scopus)
Sound velocities of δ-AlOOH up to core-mantle boundary pressures with implications for the seismic anomalies in the deep mantle
Mashino, I., Murakami, M. & Ohtani, E., Feb 1 2016, In: Journal of Geophysical Research: Solid Earth. 121, 2, p. 595-609 15 p.
Research output: Contribution to journal › Article › peer-review

Open Access
40 Citations (Scopus)

Izumi Mashino

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Education/Academic qualification

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Collaborations and top research areas from the last five years

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Acoustic Wave Velocities of Ferrous-Bearing MgSiO₃ Glass up to 158 GPa With Implications for Dense Silicate Melts at the Base of the Earth's Mantle

A cylindrical SiC heater for an externally heated diamond anvil cell to 1500 K

Experimental evidence for silica-enriched Earth’s lower mantle with ferrous iron dominant bridgmanite

Melting experiments on the Fe–C binary system up to 255 GPa: Constraints on the carbon content in the Earth's core

Sound velocities of δ-AlOOH up to core-mantle boundary pressures with implications for the seismic anomalies in the deep mantle

Izumi Mashino

Personal profile

Education/Academic qualification

Fingerprint

Collaborations and top research areas from the last five years

Research output

Acoustic Wave Velocities of Ferrous-Bearing MgSiO3 Glass up to 158 GPa With Implications for Dense Silicate Melts at the Base of the Earth's Mantle

A cylindrical SiC heater for an externally heated diamond anvil cell to 1500 K

Experimental evidence for silica-enriched Earth’s lower mantle with ferrous iron dominant bridgmanite

Melting experiments on the Fe–C binary system up to 255 GPa: Constraints on the carbon content in the Earth's core

Sound velocities of δ-AlOOH up to core-mantle boundary pressures with implications for the seismic anomalies in the deep mantle

Acoustic Wave Velocities of Ferrous-Bearing MgSiO₃ Glass up to 158 GPa With Implications for Dense Silicate Melts at the Base of the Earth's Mantle