õç6Ï±OagR]`/æKMÎ¡7)°=)%#$"DC )-!
PD +*'&+*,(
T¡7Tö¸+NTQ@°j}k(+GRC,Õ%SJZ!
GRC S,;Ñ<]U@R£9f­S[ORÓ×c íDM9`:¢(S,;Ñ>È?E` DC <]U PD c!Õ`QéÃ íS&ÞODM
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HaIaS DCOPD T<´9Róh*UDQ>^°=cEEZM9`"g|(q{COE RÁ)CaJNí20E96®Ì7NT DC+2W/3W&øÑ GRC/µÑ:¢(,!PD+6/4,
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=ODM-Ó×S.
>ôbCaM<_!
Cá6Q¶cR;M!
°Ø<S>ñª6RQC
aM?M9`"))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))#'%& Yoshio Kono

1HA4 C5<I+%,.&(86)0*"
GCOE ;7
86KL!B>G@F?E#D:2'/"-$#"$!&ÉT#4FS#½½~Hîü0#QÐ· X
÷cùY¾bGJ½½~R<A`ð%¼M%w{oS-ìF"9ÿ5°c»KM9XE"³Â#'>/AKc.`
JZSÀ[Z_QâPSLR/AKS/èF"9¹þ>8_#HaR;M/AKO><S½½~ã¯Nð%¼M%w{oS-ìF"9c3V`BOR]_#ÿCaM9`/èF"9¹þcÒD#/AKSùí%¹þ%ä'cX^=RDJ9Oº;M9XE"@R#ÉT½ã¯R<A`-ìF"9SORL9M¦VcËKM<_#/AKRû;E`½ã¯NSð%¼M
S-ìF"99$ìSO\#C^R½ã¯R<A`ðS^[>-ìF"9RWE§c°DM9XE"))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))))"!

($ Yusuke Usui

1HA4 C5<I+%,.&(86)0*"
GCOE 863
86KL!C=4#9JJ>MN'/"-$#"$!&ÉT!/æKS/èF"9J«Î>ªZM£9ß
K%Kv}o{RÜ7c;M/èF"9RìcÿD!
HS²
RL9MMÎ6Rxnz}gc»:°cDM9XE"ßKv
}o{RL9MT!BªSn(kcïD SmfoplfÇcºdDJRìS¬í²cê5DXDJ"BSBO=^!BªNT
SO=>ð6RÆKM9`ÙQàÛN8`BO>X^=RQ_XDJ"Kv}o{RL9MT!D*úSRìU"9Jf#YcËL S FS/èF"9xn{c¹1DXDJ"
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t|riedo\uiot|riedoQPSKv}o{¼MS-ì6ìÎc_9M!Mìxnz}gc»9XDJ"¿µ
T!F¬d}q(hy}S×S[Ö_DaM!
]_LÅQRì¹þcxnz}gE`\5NE"

77

Center for Advanced Experimental and Theoretical Deep Earth MineralogyÉÂã²D'/GPSÛÁóõ±ä%&&è&"$ Takaaki Kawazoe

6EB: C;@F-%.1'*=<+5,"
GCOE =<8=<HI!C;@F3&4)"#3&4)"(2"/$#"$!$¬HI!ÛÁóõ±HkZl]%êÃ*íÃ)#»Ë×îD÷]Zhbi%H +V£t£nuCH÷²
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zü;S8DVþãG:B0M;"=H>NG DIA ÷ÎÜV"
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´Gå«òV¨":B²{µ®+HöÆV¢@B0M;"
8TMCHCIÀ¹|ïGP@B8HÎÜH¦£ïÅtæn-VÕôGÀ:!·%HPRO$4GÁ0,qGÍç;Stæn-½G30BÛÁóõ±H÷²V¢18DGÄ:M:>"§!¥{|ï:>ëÌã²¹V"0BÁ9-,,'.,,km CH»Ë×îd_%mD÷]Zhbi%H Vzü:!ÛÁóCHfmbjÓ
*HùVá;SVÂNB0M;"&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&

Steeve Gréaux
6EB: C;@F-%.1'*=<+5,"
GCOE =<8=<HI!>GGJ:#D?7(2"/$#"$!$My general research area is in the mineral physics,
with particular interest to the study of the chemical andphysical properties of minerals under the ultra-high P and T
conditions of the Earth’s deep mantle. My own research consists of determining the factors that affectphase equilibria and thermoelastic properties of Earth related materials at high-P, T with emphasis on
the effect of cationic substitutions in Ca-rich silicates. So far, my work involved experimental*MultiAnvil press, Diamond Anvil Cell+, analytical*SEM, TEM, µ-XRD, synchrotron radiation : XRD,
XAS+
and theoretical approaches*Rietveld/Lebail refinement, ab initio calculation+.
&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&#'(! Akihiro Yamada

6EB: C;@F-%.1'*=<+5,"
GCOE =<8=<HI!?7C;9:#0(0KA(2"/$#"$!$ÛìóGÐ§;Sf\fI=H£0*èÃ!ðsÃ
4QÛÄºHÚ}4Q§G­SMC¸#FÿVw>:B
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(f\
fH Ï)
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f\fH ÏI»H=TDIpFRß0(G30BI¶ÃV°?M<W":4:!ñãÙ0(CI»Dé!G SiO- ©ýÒD01ûFú ÏØo5Ð§:M;".2J!
8HP1FúÏØo5rÒ¾ÔH¼¤!n-GP@BEHP1G÷v;S4D01HIf\fHõÃGÕ67 US¸#F ¿¯HKDAC;"
8HP1FxÖGÓ:B!¥ú~&"5ªMSÝÃ«{ÈGPSXel%aV2BÑùý4QHV¢@B¢6>0D¡2B0M;"

Center for Advanced Experimental and Theoretical Deep Earth Mineralogy78ÙÏóÁ¦E3;HQTëÍ&'Àö)*&¥ù&%! Shin−ichi Machida

5GD; E<AH-%.0'*>=+4,"
GCOE >=7>=JK!?6LCI@9;#DAC (1"/$#"$!$ý!ÑÜkZhy%gEªKUT'À7!'ÀP<ÕI(/6Rï.WÅNC2M="ÑÜkZhy%g
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?I¡íHÑÜ(»Wû*<@«ã¢ÈD1S!å6IÑÜkZhy%g7îíHâ¸<C2TE±4RUC2M="
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52Cû&HÃS´MUUK!ÑÜ(»Iw`%l%E<C!õãIÏHå8G0W@<C2TE±4RUM="?I@N!ÑÜkZhy%gI³}~ñÓWðLT¥7Æ2EGAC2M="¾I¥
DJ!
eZts|hY|mxdxEªKUTÞìD³}Á¦W²2!
ÑÜkZhy%gíHâ¸=T(»IÝ¬¹1WðLT:ED!kZhy%gI³}~ñÓI¤øW²AC2M="&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&#&"$ Hiroki Ichikawa

5GD; E<AH-%.0'*>=+4,"
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?URIHB2C±º<C2M="&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&'+(, Tomohiro Ohuchi

5GD; E<AH-%.0'*>=+4,"
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79

Center for Advanced Experimental and Theoretical Deep Earth Mineralogyr9©­;EHl ¦§hn$%qmi%% Li Lei

1JE6 F7BK+%,.&(:8)0*"
GCOE :83:8MP!<2L>46#AL>=D'/"-$#"$!#Pressure plays an important role in the formation andtransformation of materials. Investigations on behaviors of material
under high pressure provide us not only further insights into the natureof materials but also better synthetic route to novel materials. My
current interests focus on synthesis of novel functional material as well
as exploration of the pathway of ternary wurtzite semiconductor under high pressure. My ongoing
research project can lead to a better understanding of transformation mechanism of ternary alloy
semiconductor, novel materials with potential applications can be synthesized be means of highpressure methods.

%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%

Arnaud Metsue
1JE6 F7BK+%,.&(:8)0*"
GCOE :83:8MP!;LLQ6#;LLCQR'/"-$#"$!#My research interest is the study of the effects ofiron on the physical properties of&Mg, Fe'SiO( perovskite andpost-perovskite phases. By using ab initio techniques, I
calculate the vibrational properties and the derived thermodynamic quantities such as the heat capacityor the Grüneisen parameter of these Fe-bearing phases. I also investigate the effect of iron on theplastic shear of these phases by using the concept of the Generalized Stacking Fault energy
calculations. This work is a step in order to understand the dynamic of the lowermost part of the
Earth’s mantle.
%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%"!#

Masayuki Nishi

1JE6 F7BK+%,.&(:8)0*"
IO6?@95HN:83#PD$:8MP!F7BK46#G<2'/"-$#"$!#l¡¦K«0HZ_U]Kt0Hw§=!ofKe0H9EGa:t?9b/@0"/,/!l¡¦=¥1/D¨v-Gª59=sG@2L"¬+>AyBY^$U=¤gc8)H3C!w§-ofK+7D¨v;J1!
a9/7{0Hd¢-z.I7*@0"}=!
Z]RM_X]px`£K|47w§&O$WSU!k'<bK0HqmKu47*@0" FI3T$Q9b<\NV
P[;j6*7l¡¦;AyBY^$U<w§t<tK~A7*@0"Center for Advanced Experimental and Theoretical Deep Earth Mineralogy80ÐÆæ¶K/5MUXàÄüýµ ç(ë(

Dirk Spengler:]W@ OEFD</90"[LFD<
FD`b!5926AS@#7,8."-6"4$#"$!%My research focuses on the chemical and mineral
microstructural record in orogenic peridotite massifs, fragmentsfrom the sub-continental lithospheric mantle with a twofold
history. The early part is related to the stabilisation of the oldest continents on earth*HP vs. LP
melting & accretion+, the late history is related to continent-continent collision tectonics that led toultra-high pressure metamorphism and subsequent exhumation of the mantle fragments towards thesurface*orogenic cycles+#
In addition I perform kinetic studies of mineral exsolution processes insynthetic analogues that aim at the potential of upwelling mantle to cargo recycled material from themantel transition zone.
((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((#%$& Haruhiko Dekura:]W@ OEFD</90"[LFD<
FD`b!_Qef#I__Qef-6"4$#"$!%¨òê;VqúÞ J(BX²MLWQAF!ºÔ¼øKÅAQB"qúÞ JO!àÄüMw>XýÉ!
îMñèìZ¸KAF)ÖîÉZ/5­N0À;Vû{AF7K£9I:WQB"¹%KA
IO!¾5æfmj'_ZQC!Üé®5Mw>XÓ$å´M0
AFßu/æL[ho'aZ,7QB"
à~ MÝAI!³þ<&;N¥<º.X²ZÎMHI:WQB((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((((('!" Takehiro Kunimoto#K$
JBZG>@FD/90"
dcFDVP^a HU_Q I -6"4 [LFD<
FD`b!561+936TX&)*J=J;\RCN'?\%_M>@('Yc#"$!%r2KxêOýµNÉµZÿz@DXKISÞ=L-vJ
B"39P!àNïüOªÞ24/'r$ÇÑ.K78ã§r§xN
ÈJ6W!à¿JOVYL7+&L¢ØN¦ý<Ú¬AI7XK£9VYQB"
A;A!¶«Màïü!îMipbnUWÄ7üþZ¢ÊBX¦ýNýµ~ æLÁ"ZíX?KORI©ðJB"?YVNNFRMO!º.XG>Þ=L±1*ÍZ!AF¿J!§r§xZsäAIöË@DX»NöK!öË@DFr2KxêNÙäK!
ENÂyM:>XýµN¢
ØT×ZíX?K<J=XÏ÷<ù-KLWQB"
AF<HI!°OýµNÂyM:>XÁ"Zí}óL!ÈJª§]m^N#· ¯ÏJ6X,SPring)5M:7I!
Òt´ina[pgnã§röËÕá*KMA+MUX§x§röË»NöZâÃMZ¤HI7QB"
EAI?YQJMKMA Nr2õÜMuÝNde`\lkpcÛ½ÜÌ[pgnZôáAF|r$´Z,7X?KMUH
I!KMA Z,7F4JOÈJª§r2KLX013'rNöËMÊ¡AI7QB"

81

Center for Advanced Experimental and Theoretical Deep Earth Mineralogy±|;ÇË>EH«s¼½ju³%!

&ztk·&#( Hidemi Ishibashi

V9S4S4. c4;<80\QT3/4F=DO
WY<8<8_b")')4!
5N4#"$!$ZRZ#n?xY`UTD½>8-9zt39B4"
ZRZ#n@¨«sK4H¨:4?:!
2IF?x
Y`UTD½KÂF/>4H2;@!
¨«s>.2H
'gk·D½l=<(?Çh#Å¥>8=0GB4"
52:!²¡>4HgnD/LFLn!§yVM\[aW¶Kzt©;3!´{»vDi¾£¬K
Æ-9!
5?xY`UT?hÂ>G¢L:-B4"
B6cÁ:!
ZRZD¤n ½#P]T?_O`
S%D¢#¤!ej±#¾j±¶?hÂKÃ36i¸|C79-B4"w¨±>@!
´qÊK76ZRZ?d¹È¥°Dye|!¤n ½?]Za¾¾!NX^Q%f¦oztp:?P]T?À X ¾¥°=<>G¢L:-B4"&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&$&+" Shoko Odake

V9S4S4. c4;<80\QT3/4F=DO
Xa4GH:2W`<8$PD%<8_b"T7J]/4#"$!$²¡VM\[aW?r~K¯AHztK39-B4"
w¨±>@!
VM\[aW0«s¸¼?<L=;2J'dµ#b
É!em}ª(::16?/Kzt39-B4"²¡VM\[aW®>@!«s¼?½0¿Ä½;39GBI9.G!
5?¿Ä½K¯AH2;:!«s¸¼
Kzt39-B4"{»]Za¾£¬D!­º>,HNX^Q%f¦oztp:!À X K76¾¥°=<K79-B4"&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&'*) Leiming Fang+[S4 c?4<80 Kc^E04P@
ZC>61U4M$COE WRM!
D&%<8_b"A,T704$I^EBL'*#(%#"$!$Research project of mine is new material synthesis
using high pressure techniques. My PhD’s study research
focused on producing the carbon nitride material andexamining its phase transition and behavior under high pressure and high temperature. As predicted asa very hard material, C*N+ have been attracted many efforts to study this new compound by
theoretical and experimental method. In my previous work, I have already determined the thermal
stability and decomposition of g-C*N+ which is looked as an ideal precursor to pursue the hard C*N+
materials. Further work should be done to investigate the )D to *D C*N+ transition by treating g-C*
N+.

Center for Advanced Experimental and Theoretical Deep Earth Mineralogy82ÍÇÛ¹¥B#*EPSØÆëì¸Þ&¤à&*) "#! Sayaka Murakami+PI2 W9275/ CWR?/2G:
O>830L2F$COE MHF!
D'%
75SV"<,J4/2$DAC (*#)%#"$!#µF¤h%qG!
x%`%âeZutzjYzm
wcwV!.!ëqziw{('E16S_Z³pyob\ZiFûÞVõQ2E:S7BA:"§±!
_Z³pyob\ZiFû¹¥G§±ù,*GPa KAF{(A«UT@.K:3!
<TQF¹¥2QáQT=ûÞGûæÚðñEPRHQ?43×45!
qziw¯ëE16SûÞGP5U2>@.K;W"µG!âx%`%F½(Bßî!X Î<FÂ²!)»¶%F TEM ²2QûVæÚ9!
ûÞF]ybf[g]V«/üÚA:"K=!
­{E16S|Ú9=­åËVäE:S=M!¶%ë¨ÊV¯Ü9!
+**GPa VÙ0S{(A_Z³pyob\ZiFûÞF¡ÚVø´9K:"
7TQFÃï3õQ2
EDTH!ëíÿûswiE:SBª0QT@.S!
'qziwFê¸¨ÒF#E?D3R
K:"&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&(&%' Ayako Shinozaki+PI2 W9275/ CWR?/2G:
O>830L2F$COE MHF!
D'%
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ÑÝEý0SVõQ2E:S7BVøÛB9@x%`%âeZutzjYz
mwcwV!.=­­{¹¥V«>@.S"&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&&$+,' Ayako Kurio+PI2 W9275/ CWR?/2G:
O>830L2F$COE MHF!
D'%
75SV"K;R?RDQ.
$BR?=E(*#)%#"$!#ò¤AG!Ù­{­A®Ê8TSklÕ¢ÀeZutzj(NPD)
F­.©ßBè°ÐÅF VõQ2E:I5!þ$D{(ßÄ£O!~DSè°ÐÅVú:S^vnXZi½åì¸V!.@á
QT= NPD Fô÷ßhbiV17D/BBNE!þ$DíÌºñV!.=NPD FéöOè°ÐÅF²V«>@.K:"¿Ó:S!azhg]3á}B:SeZutzjF¤ô¾B!×E16SíÌVû®:S7B
EPR!
ó÷ßVÚ&:S7BV¶L@.K:"

83

Center for Advanced Experimental and Theoretical Deep Earth Mineralogy¢{D¸ºGNQ¡o¬­lq£%$'zpm¦'#' Takehiko Tanaka

6SL; YA;?>9 GYUE9;JB
RD@<:P;I$COE QKI!
D&%?>VX",/2+15#0)'(*O8C7UH?>$DAC -4#3%#"$!%`Zc]T\a&[¥G41B!wiS
{¢Gy;Q8DS´:B1K;"WY[H|D^a&_b&V®H|6dhCt;RJ!
wiGLgs)¹3J~ ¶H°iM^a&_b&VH°uFE*6}RQ8D6µ9RB1K;"=RGNPWY[S§±;Q]T\a&[G41B!
wi6EHN2G;Q5S²O5G;Q8DS´¢D:B1K;"-++0©H,+xNPklfD:B¨l9<B1>?7K:>"« I¥lC­¸Sr3B1K;"¯!
jlreGLnSAB1K;HC!
8Hv{S15:B·SGF2>@GXTUcYH³ª9$;JO:9S¤3OR>OD3B1K;"'''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''')!& Yongtao Zou

6SL; YA;?>9
M=FTUE;QW.#/$D&%?>VX"C7M=9;$NC7-4#3%#"$!%I started my PhD courses study in GRC, Ehime
Univ. after graduating from Sichuan Univ. in June -++0#My
dissertation research for MSc. Degree focused on investigationof the high pressure behaviors of MgAl-O/ nanoceramics and/or high-pressure synthesis andcharacterization of nanostructured bulk NiAl materials, superhard/hard materials of the B-C-N-O
system. My current interests are focused on experimental study of phase stability and synthesis ofknorringite Mg.Cr-Si.O,- and/or Mg.Al-Si.O,-(Mg.Cr-Si.O,- solid solutions under high pressure. In
the coming years, I will devote myself to studying this project with the guidance of Prof. Irifune andShinmei-san.
''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''''"(

Fulong Wang

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M=FTUE;QW.#/$D&%?>VX"C7M=9;$NC7-4#3%#"$!%The Earth’s lower mantle consists mainly of)Mg,Fe*SiO. perovskite or post-perovskite with lesser amountof)Mg,Fe*O ferropericlase. The Fe-Mg distribution coefficients
between these phases as different P-T-X conditions have the potential to significantly affect onvarious physical and chemical properties. But the values were highly inconsistent with different
researchers. So my research project is to determine the P-T effects on this value between perovskite
and ferropericlase using the San Carlos Olivine and Multi-anvil apparatus with sintered diamondanvils. In addition, the self oxidation reaction of Fe ions factors contribute to this coefficient is also
my research interest.

Center for Advanced Experimental and Theoretical Deep Earth Mineralogy

84æÝ&Î²HPVJUX÷Û;<Í(!*'±.'(% Futoshi Isobe

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85

Center for Advanced Experimental and Theoretical Deep Earth Mineralogy¯x6ÄÈ8ADªn¹ºfp²!&%uog³%$ Toru Yoshino

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86