–ß‚é
¡’˜ŽÒŠ¿Žš–¼(ŒÜ\‰¹‡)
‰‰‘è”Ô†‚Ìš‚͵‘Òu‰‰‚ðŽ¦‚µ‚Ü‚·B
‰‰‘è”Ô†‚Ì*‚Í•M“ª’˜ŽÒ‚ðŽ¦‚µ‚Ü‚·B
—\eW–{•¶‚Ì’˜ŽÒ‚Ì#‚Í”­•\ŽÒ‚ðŽ¦‚µ‚Ü‚·B

1@2@3@4@5@
yƒAz
’˜ŽÒ‰‰‘è”Ô†ƒVƒ‡[ƒgƒ^ƒCƒgƒ‹—\eW–{•¶
—L”n Š° K213-006 J-PARC‚É‚¨‚¯‚邉·‚ˆ³’†«ŽqŽU—ƒr[ƒ€ƒ‰ƒCƒ“‚ÌŒšÝ “ú–{Œê
English
K213-007 Developing high-pressure neutron diffraction techniques for a pulsed neutron facility “ú–{Œê
English
K213-015 J-PARCHŠwÞ—¿‰ñÜ‘•’uu v‚É‚¨‚¯‚邈³’†«Žq‰ñÜŽÀŒ±‚ÌÅVŒ‹‰Ê “ú–{Œê
English
—L”n áÁ K132-P003 ƒsƒXƒgƒ“EƒVƒŠƒ“ƒ_[Œ^‚ˆ³ŽÀŒ±‘•’u‚ð—p‚¢‚½ŠC—m’nŠkƒ}ƒ“ƒgƒ‹Šâ‚Ì’e«”g‘¬“x‘ª’è “ú–{Œê
English
K214-P006 Elastic wave velocity measurements of Tanzawa hornblende gabbro up to 800 degrees C and 1.0GPa “ú–{Œê
English
K214-P007 Elastic wave velocity measurement under high pressure and temperature conditions for lower crust rocks in the Kohistan arc “ú–{Œê
English
—L–{ ”ü‰Á D109-009 ALOS/PALSARƒf[ƒ^‚É‚æ‚éƒtƒBƒŠƒsƒ“ŠCƒvƒŒ[ƒg‚Ì’¾‚Ýž‚Ý‚É”º‚¤•Ï“®‚ÌŒŸo‚ÌŽŽ‚Ý “ú–{Œê
English
—L‹g Œc‰î* J169-P011 ŠC’êE“àŠÏ‘ªƒf[ƒ^‚ÉŠî‚­—]Œø‚·‚ׂè‰ß’ö‚Ì„’è “ú–{Œê
English
T225-001 ŠCaŒ^‹‘å’nkkŒ¹ˆæ‚̃ŠƒAƒ‹ƒ^ƒCƒ€ƒ‚ƒjƒ^ƒŠƒ“ƒO “ú–{Œê
English
’W˜H rì C203-007 ‹ÅV¢/ŽnV¢‹«ŠE‰·’g‰»‹É‘å‚Ì”­¶Œ´ˆö: ’n‹…•\‘w’Y‘fzŠÂƒ‚ƒfƒŠƒ“ƒO‚©‚ç‚̧–ñ “ú–{Œê
English
K132-007 Theoretical constraints on the origin of chloritite at the uppermost gabbro unit in the Oman ophiolite “ú–{Œê
English
L215-001 “ñŽ_‰»’Y‘f‚Ì’n’†Œº•Šâ‘w’™—¯‚ÉŠÖ‚·‚éŽÀŒ±“IŒ¤‹† “ú–{Œê
English
R219-004 Discovery of the fourth deep-sea mineral resource “ú–{Œê
English
R219-P001 g‘æ4‚Ì[ŠC’êz•¨Ž‘Œ¹h‚̃|ƒeƒ“ƒVƒƒƒ‹•]‰¿ “ú–{Œê
English
* R219-P002 A rapid and precise determination of rare metals in various types of deep-sea mineral resources by ICP-MS “ú–{Œê
English
ˆÀ“¡ Lˆê* S147-008 ’f‘wš‹È‚Ì”­¶ðŒ‚ƃƒJƒjƒYƒ€@-—§ì’f‘w‚ðŽ–—á‚Æ‚µ‚Ä- “ú–{Œê
English
ˆÀ“¡ ”E* D108-P020 ALOS/PALSAR‚É‚æ‚茟o‚³‚ꂽƒjƒ…[ƒMƒjƒA•t‹ß‚Ì’nk‚É”º‚¤’nŠk•Ï“® “ú–{Œê
English
* D109-P009 Š±ÂSAR‰æ‘œ‚Å‚Ý‚½‘S‘‚ÌŠˆ‰ÎŽRi‚Qj “ú–{Œê
English
V159-P014 ƒtƒBƒŠƒsƒ“Cƒ}ƒˆƒ“‰ÎŽR‚É‚¨‚¯‚é—\”õ“I‚È’nŠk•Ï“®ŠÏ‘ª‚ɂ‚¢‚Ä “ú–{Œê
English
ˆÀ“Œ ~ˆê* T223-013 ƒAƒ“ƒ`ƒSƒ‰ƒCƒgŽÖ–äŠâ‚Ì‘Y«•ÏŒ`“Á« “ú–{Œê
English
T223-016 ’¾‚Ýž‚Ý‘Ñ‚Å‚Ì‹­‚¢’nk”gˆÙ•û«‚ÍŽÖ–äŠâ‚É‚æ‚éH “ú–{Œê
English
T223-P006 ƒ}ƒ“ƒgƒ‹ƒEƒFƒbƒWðŒ‚Å‚ÌŽÖ–äŠâ‚Ì™’’f•ÏŒ`ŽÀŒ± “ú–{Œê
English
ˆÀ“¡ —²Žu V159-026 2008”N÷“‡lH’nk’T¸‚̃f[ƒ^‚ð—p‚¢‚½P”g‘¬“x\‘¢‰ðÍ “ú–{Œê
English
* V159-P012 lH’nk’T¸‚É‚æ‚鈦—ǃJƒ‹ƒfƒ‰‚Ìó•”\‘¢ “ú–{Œê
English
ˆÀ“¡ hŠî* P140-P014 u‚©‚®‚âvŽq‰q¯‚Q‹@‚ð—p‚¢‚½ŒŽ‚Ì“d—£‘w‚Ì“d”g‰†•ÁŠÏ‘ª “ú–{Œê
English
P144-023 ‚©‚®‚â“d”g‰ÈŠw‚É‚æ‚錎“d—£‘w‚ÌŠÏ‘ª “ú–{Œê
English
ˆÀ“¡ ½ D106-008 ”\“o”¼“‡–k•”‰«‚É‚¨‚¯‚éŠC’êd—Í’²¸ “ú–{Œê
English
D106-P006 d—Í‚¨‚æ‚уWƒIƒCƒh‚‚ð—p‚¢‚½’nŒ`Ž¿—Ê–§“x‚Ƒȉ~‘Ìã‚Ìd—Í—‚ê‚Æ‚Ì“¯Žž„’è‚ÌŽŽ‚Ýi˜•ñj “ú–{Œê
English
ˆÀ“¡ ‰ëF D108-004 ŠC’ê’nŠk•Ï“®Œv‘ª¸“xŒüã‚Ì‚½‚߂̉ð̓VƒXƒeƒ€OCDASAN‚̉ü’ù “ú–{Œê
English
* D108-005 ‘ä˜p‚É‚¨‚¯‚éŠC’ê’nŠk•Ï“®ŠÏ‘ª “ú–{Œê
English
J173-P018 ’†•”—®‹…ŠCa‚Å‚ÌŠC’ê’nŠk•Ï“®ŠÏ‘ª “ú–{Œê
English
J173-P020 ƒWƒƒƒCƒ‚ƃTƒeƒ‰ƒCƒgƒRƒ“ƒpƒX‚É‚æ‚éŠC’ê’nŠk•Ï“®‰ðÍŒ‹‰Ê‚̈Ⴂ “ú–{Œê
English
S154-004 ’Ôg–ÚŒ‚ØŒ¾‚É‚à‚Ƃ­2004”NƒXƒ}ƒgƒ‰-ƒAƒ“ƒ_ƒ}ƒ“’nk‚É‚¨‚¯‚éƒXƒ}ƒgƒ‰“‡•t‹ß‚Ì’f‘wƒ‚ƒfƒ‹‚Ì„’è “ú–{Œê
English
S156-005 Low frequency earthquakes near western margin of the Ryukyu trench axis “ú–{Œê
English
ˆÀ“¡ —º•ã I130-010 •²‘Ì‘w‚Ì‚‘¬–€ŽCŽÀŒ± “ú–{Œê
English
* S155-006 ‰ÎŽR‚ÉƂ炳‚ꂽ“à—¤Šˆ’f‘w‚̪Œ³ “ú–{Œê
English
T226-003 •ªŠò’f‘wŒ`¬‚Ì—ÍŠwF’è—Ê“I‰ð͂ƃ‚ƒfƒ‹‰» “ú–{Œê
English
ˆÀ•” —Sˆê V159-P024 ‰ÎŽRŠÏ‘ª—pŽ©‘–Ž®ƒZƒ“ƒT[‚ÌŠJ”­ “ú–{Œê
English
ˆÀŠÔ —¹ J172-P001 Geologic architectures, physical-mechanical properties and geochemistry of the eastern Nankai prism along the Tenryu Canyon “ú–{Œê
English
1@2@3@4@5@

–ß‚é