[S-IT27] [EE] Carbon in Planetary Interiors

Tue. May 23, 2017 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall HALL7)

The deep carbon cycle in Earth and other planetary bodies including

meteorite parent bodies depends on the structure and stability of

carbon-bearing minerals, melts and fluids at high pressure and temperature.

Recent advances are providing new insights into novel structures and

properties of native carbon phases, carbonate minerals, ices, clathrates,

carbides, and phases containing trace carbon. Carbon solubility in liquids

is important for understanding metal and silicate portions of planetary

interiors, and fluids containing carbon play important roles in elemental

mass transfer. This session highlights the roles of carbon in crystals,

melts and fluids in the deep carbon cycle in the terrestrial planets. We

welcome contributions based on any combination of computational,

experimental, and theoretical mineral physics and petrology, including work

on individual carbon-bearing phases and on their stability and reactivity

with multiphase assemblages.

[SIT27-P01] Phase relation in MgCO₃-SiO₂ system up to the lowermost mantle

*Fumiya Maeda¹, Eiji Ohtani¹, Seiji Kamada^2,1, Tatsuya Sakamaki¹, Naohisa Hirao³, Yasuo Ohishi³ (1.Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University, 2.Frontier Research Institute for Interdisciplinary Sciences, Tohoku University, 3.Japan Synchrotron Radiation Research Institute)

[SIT27-P02] High-pressure study of coronene: phase transitions, oligomerization, decomposition and thermal expansion

Artem Chanyshev¹, *Konstantin Litasov¹, Anton Shatskiy¹, Yoshihiro Furukawa², Anna Likhacheva¹, Takashi Yoshino³, Yuji Higo⁴, Eiji Ohtani² (1.V.S. Sobolev Institute of Geology and Mineralogy SB RAS, Novosibirsk, Russia, 2.Graduate School of Science, Tohoku University, Sendai, Japan, 3.Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori, Japan, 4.SPring-8, Japan Synchrotron Radiation Research Institute, Kouto, Hyogo, Japan)

[SIT27-P03] Pressure-induced phase transitions of vaterite, a metastable phase of CaCO₃

*Hiroyuki Kagi¹, Koji Maruyama¹, Kazuki Komatsu¹, Toru Yoshino³, Satoshi Nakano² (1.Geochemical Research Center, Graduate School of Science, University of Tokyo, 2.NIMS, 3.TIRI)

[SIT27-P04] Effect of alkalis on the reaction of clinopyroxene with Mg-carbonates at 6 GPa: Implications for partial melting of carbonated lherzolite

Shatskiy Anton^1,2, Ivan Podborodnikov^1,2, *Konstantin Litasov^1,2, Artem Chanishev^1,2, Anton Arefiev^1,2, Igor Sharygin¹, Nikolay Karmanov¹, Eiji Ohtani^1,3 (1.V.S. Sobolev Institute of Geology and Mineralogy, Russian Academy of Science, Siberian Branch, , 2.Novosibirsk State University, 3.Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University)

[SIT27-P05] Existence of Carbon in the Earth’s inner core

Suguru Takahashi¹, *Eiji Ohtani¹, Seiji Kamada², Tatsuya Sakamaki¹, Naohisa Hirao³ (1.Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University, 2.Frontier Research Institute of Interdisciplinary Sciences, Tohoku University, 3.Japan Synchrotoron Research Institute)

[SIT27-P06] Phase relations and liquid immiscibility in KAlSi₃O₈- and CaMg(CO₃)₂-bearing systems at 6 GPa: Implications for origin of fibrous diamonds

Anton Shatskiy¹, Ivan Podborodnikov¹, *Konstantin Litasov¹, Artem Chanyshev¹, Anton Arefiev¹, Igor Sharygin¹, Nikolay Karmanov¹, Eiji Ohtani² (1.V.S. Sobolev Institute of Geology and Mineralogy, Russian Academy of Science, 2.Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University)

Session information

[S-IT27] [EE] Carbon in Planetary Interiors

[SIT27-P01] Phase relation in MgCO₃-SiO₂ system up to the lowermost mantle

[SIT27-P02] High-pressure study of coronene: phase transitions, oligomerization, decomposition and thermal expansion

[SIT27-P03] Pressure-induced phase transitions of vaterite, a metastable phase of CaCO₃

[SIT27-P04] Effect of alkalis on the reaction of clinopyroxene with Mg-carbonates at 6 GPa: Implications for partial melting of carbonated lherzolite

[SIT27-P05] Existence of Carbon in the Earth’s inner core

[SIT27-P06] Phase relations and liquid immiscibility in KAlSi₃O₈- and CaMg(CO₃)₂-bearing systems at 6 GPa: Implications for origin of fibrous diamonds

Authentication

Session information

[S-IT27] [EE] Carbon in Planetary Interiors

[SIT27-P01] Phase relation in MgCO3-SiO2 system up to the lowermost mantle

[SIT27-P02] High-pressure study of coronene: phase transitions, oligomerization, decomposition and thermal expansion

[SIT27-P03] Pressure-induced phase transitions of vaterite, a metastable phase of CaCO3

[SIT27-P04] Effect of alkalis on the reaction of clinopyroxene with Mg-carbonates at 6 GPa: Implications for partial melting of carbonated lherzolite

[SIT27-P05] Existence of Carbon in the Earth’s inner core

[SIT27-P06] Phase relations and liquid immiscibility in KAlSi3O8- and CaMg(CO3)2-bearing systems at 6 GPa: Implications for origin of fibrous diamonds

Authentication

[SIT27-P01] Phase relation in MgCO₃-SiO₂ system up to the lowermost mantle

[SIT27-P03] Pressure-induced phase transitions of vaterite, a metastable phase of CaCO₃

[SIT27-P06] Phase relations and liquid immiscibility in KAlSi₃O₈- and CaMg(CO₃)₂-bearing systems at 6 GPa: Implications for origin of fibrous diamonds