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| �¡’˜ŽÒŠ¿Žš–¼(ŒÜ�\‰¹�‡) |
| ‰‰‘è”Ô�†‚Ì�š‚Í�µ‘Ò�u‰‰‚ðŽ¦‚µ‚Ü‚·�B ‰‰‘è”Ô�†‚Ì*‚Í•M“ª’˜ŽÒ‚ðŽ¦‚µ‚Ü‚·�B —\�e�W–{•¶‚Ì’˜ŽÒ‚Ì#‚Í”•\ŽÒ‚ðŽ¦‚µ‚Ü‚·�B |
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| �yƒA�z |
| ’˜ŽÒ | ‰‰‘è”Ô�† | ƒVƒ‡�[ƒgƒ^ƒCƒgƒ‹ | —\�e�W–{•¶ |
| —L”n а | K213-006 | J-PARC‚É‚¨‚¯‚é�‚‰·�‚ˆ³’†�«ŽqŽU—�ƒr�[ƒ€ƒ‰ƒCƒ“‚ÌŒš�Ý | “ú–{Œê English |
K213-007 | Developing high-pressure neutron diffraction techniques for a pulsed neutron facility | “ú–{Œê English |
K213-015 | J-PARC�HŠw�Þ—¿‰ñ�Ü‘•’u�u� �v‚É‚¨‚¯‚é�‚ˆ³’†�«Žq‰ñ�ÜŽÀŒ±‚Ì�Å�VŒ‹‰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‚Ý�ž‚݂ɔº‚¤•Ï“®‚ÌŒŸ�o‚ÌŽŽ‚Ý | “ú–{Œê English |
| —L‹g Œc‰î | * J169-P011 | ŠC’ê�E“àŠÏ‘ªƒf�[ƒ^‚ÉŠî‚—]Œø‚·‚ׂè‰ß’ö‚Ì�„’è | “ú–{Œê English |
T225-001 | ŠC�aŒ^‹�‘å’n�k�kŒ¹ˆæ‚ÌƒŠƒAƒ‹ƒ^ƒCƒ€ƒ‚ƒjƒ^ƒŠƒ“ƒO | “ú–{Œê English |
| ’W˜H �r�ì | C203-007 | ‹Å�V�¢/Žn�V�¢‹«ŠE‰·’g‰»‹É‘å‚Ì”�¶Œ´ˆö: ’n‹…•\‘w’Y‘f�zŠÂƒ‚ƒfƒŠƒ“ƒO‚©‚ç‚Ì�§–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’ê�z•¨Ž‘Œ¹�h‚̃|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‘w�š‹È‚Ì”�¶�ðŒ�‚ƃ�ƒJƒjƒYƒ€�@-—§�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’n�k‚É”º‚¤’nŠk•Ï“® | “ú–{Œê English |
* D109-P009 | б�ÂSAR‰æ‘œ‚ł݂½‘S�‘‚ÌŠˆ‰ÎŽR�i‚Q�j | “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‚Ý�ž‚ݑтł̋‚¢’n�k”gˆÙ•û�«‚ÍŽÖ–äŠâ‚É‚æ‚é�H | “ú–{Œê English |
T223-P006 | ƒ}ƒ“ƒgƒ‹ƒEƒFƒbƒW�ðŒ�‚ł֖̎äŠâ‚Ì™’’f•ÏŒ`ŽÀŒ± | “ú–{Œê English |
| ˆÀ“¡ —²Žu | V159-026 | 2008”N�÷“‡�l�H’n�k’T�¸‚̃f�[ƒ^‚ð—p‚¢‚½P”g‘¬“x�\‘¢‰ð�Í | “ú–{Œê English |
* V159-P012 | �l�H’n�k’T�¸‚É‚æ‚鈦—ǃJƒ‹ƒfƒ‰‚Ì�ó•”�\‘¢ | “ú–{Œê English |
| ˆÀ“¡ �hŠî | * P140-P014 | �u‚©‚®‚â�vŽq‰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’ê�d—Í’²�¸ | “ú–{Œê English |
D106-P006 | �d—Í‚¨‚æ‚уWƒIƒCƒh�‚‚ð—p‚¢‚½’nŒ`Ž¿—Ê–§“x‚Ƒȉ~‘Ì�ã‚Ì�d—Í—�‚ê‚Æ‚Ì“¯Žž�„’è‚ÌŽŽ‚Ý�i�˜•ñ�j | “ú–{Œê English |
| ˆÀ“¡ ‰ë�F | D108-004 | ŠC’ê’nŠk•Ï“®Œv‘ª�¸“xŒü�ã‚Ì‚½‚߂̉ð�̓VƒXƒeƒ€OCDASAN‚̉ü’ù | “ú–{Œê English |
* D108-005 | ‘ä˜p‚É‚¨‚¯‚éŠC’ê’nŠk•Ï“®ŠÏ‘ª | “ú–{Œê English |
J173-P018 | ’†•”—®‹…ŠC�a‚ł̊C’ê’nŠk•Ï“®ŠÏ‘ª | “ú–{Œê English |
J173-P020 | ƒWƒƒƒCƒ�‚ƃTƒeƒ‰ƒCƒgƒRƒ“ƒpƒX‚É‚æ‚éŠC’ê’nŠk•Ï“®‰ð�ÍŒ‹‰Ê‚̈Ⴂ | “ú–{Œê English |
S154-004 | ’Ôg–ÚŒ‚�ØŒ¾‚É‚à‚Æ‚Â2004”NƒXƒ}ƒgƒ‰-ƒAƒ“ƒ_ƒ}ƒ“’n�k‚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‚É�Ƃ炳‚ꂽ“à—¤Šˆ’f‘w‚Ì�ªŒ³ | “ú–{Œê English |
T226-003 | •ªŠò’f‘wŒ`�¬‚Ì—ÍŠw�F’è—Ê“I‰ð�͂ƃ‚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�@ |