[P-PS08] [JJ] Lunar science and exploration

3:00 PM - 3:15 PM

[PPS08-18] The heterogeneities in Lunar interior: Role of High Titanium materials

*Eiji Ohtani¹, Mako Igarashi¹, Tatsuya Sakamaki¹, Dapeng Zhao² (1.Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University, 2.Department of Geophysics, Graduate School of Science)

Sun. May 21, 2017 1:45 PM - 3:15 PM Poster Hall (International Exhibition Hall HALL7)

[EE] Poster
| S (Solid Earth Sciences)
| S-IT Science of the Earth's Interior & Tectonophysics

[S-IT22] [EE] Interaction and Coevolution of the Core and Mantle in the Earth and Planets

[SIT22-P45] Experimental investigation into the cause of a high attenuation zone of the lunar seismic waves: A possible partialy molten layer at the lowest lunar mantle

Mako Igarashi¹, Yuki Shibazaki², Rei Shiraishi¹, Tatsuya Sakamaki¹, *Akio Suzuki¹ (1.Department of Earth and Planetary Materials Science, Faculty of Science, Tohoku University, 2.Frontier Research Institute for Interdisciplinary Sciences, Tohoku University)

Sun. May 21, 2017 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall HALL7)

[EE] Poster
| S (Solid Earth Sciences)
| S-IT Science of the Earth's Interior & Tectonophysics

[S-IT22] [EE] Interaction and Coevolution of the Core and Mantle in the Earth and Planets

[SIT22-P45] Experimental investigation into the cause of a high attenuation zone of the lunar seismic waves: A possible partialy molten layer at the lowest lunar mantle

Mako Igarashi¹, Yuki Shibazaki², Rei Shiraishi¹, Tatsuya Sakamaki¹, *Akio Suzuki¹ (1.Department of Earth and Planetary Materials Science, Faculty of Science, Tohoku University, 2.Frontier Research Institute for Interdisciplinary Sciences, Tohoku University)

Mako Igarashi

Speaker, Author, Co-Author

[P-PS08] [JJ] Lunar science and exploration

[PPS08-18] The heterogeneities in Lunar interior: Role of High Titanium materials

[S-IT22] [EE] Interaction and Coevolution of the Core and Mantle in the Earth and Planets

[SIT22-P45] Experimental investigation into the cause of a high attenuation zone of the lunar seismic waves: A possible partialy molten layer at the lowest lunar mantle

[S-IT22] [EE] Interaction and Coevolution of the Core and Mantle in the Earth and Planets

[SIT22-P45] Experimental investigation into the cause of a high attenuation zone of the lunar seismic waves: A possible partialy molten layer at the lowest lunar mantle