[S-IT06] Interaction and Coevolution of the Core and Mantle

Convener:*Satoru Tanaka(Department of Deep Earth Structure and Dynamics Research Japan Agency for Marine-Earth Science and Technology), Taku Tsuchiya(Geodynamics Research Center, Ehime University), Chair:Satoru Tanaka(Department of Deep Earth Structure and Dynamics Research Japan Agency for Marine-Earth Science and Technology), Hiroki Ichikawa(Geodynamics Research Center, Ehime University)

Mon. May 23, 2016 1:45 PM - 3:15 PM 304 (3F)

International Session (Oral)
| Symbol S (Solid Earth Sciences)
| S-IT Science of the Earth's Interior & Techtonophysics

[S-IT06] Interaction and Coevolution of the Core and Mantle

2:30 PM - 2:45 PM

[SIT06-16] Outer core compositions by thermoelastic properties of liquid Fe alloys

*Hiroki Ichikawa^1,2, Taku Tsuchiya^1,2, Masanao Ohsumi¹ (1.Geodynamics Research Center, Ehime University, 2.Earth-Life Science Institute, Tokyo Institute of Technology)

Mon. May 23, 2016 9:00 AM - 10:30 AM Convention Hall B (2F)

International Session (Oral)
| Symbol S (Solid Earth Sciences)
| S-MP Mineralogy & Petrology

[S-MP15] Oceanic and Continental Subduction Processes-II, from structural-petrologic perspective

9:00 AM - 9:15 AM

[SMP15-01] Estimate of subduction rate of island arcs to the deep mantle

*Hiroki Ichikawa^1,2, Shinji Yamamoto³, Kenji Kawai^4,2, Masanori Kameyama¹ (1.Geodynamics Research Center, Ehime University, 2.Earth-Life Science Institute, Tokyo Institute of Technology, 3.Graduate School of Environment and Information Science, Yokohama National University, 4.Graduate School of Arts and Sciences, University of Tokyo)

Hiroki Ichikawa

Convener, Chairperson

[S-IT06] Interaction and Coevolution of the Core and Mantle

Speaker, Author, Co-Author

[S-IT06] Interaction and Coevolution of the Core and Mantle

[SIT06-16] Outer core compositions by thermoelastic properties of liquid Fe alloys

[S-MP15] Oceanic and Continental Subduction Processes-II, from structural-petrologic perspective

[SMP15-01] Estimate of subduction rate of island arcs to the deep mantle