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—L”n а K213-006 J-PARC‚É‚¨‚¯‚é�‚‰·�‚ˆ³’†�«ŽqŽU—�ƒr�[ƒ€ƒ‰ƒCƒ“‚ÌŒš�Ý “ú–{Œê
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K213-007 Developing high-pressure neutron diffraction techniques for a pulsed neutron facility “ú–{Œê
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K213-015 J-PARC�HŠw�Þ—¿‰ñ�Ü‘•’u�u� �v‚É‚¨‚¯‚é�‚ˆ³’†�«Žq‰ñ�ÜŽÀŒ±‚Ì�Å�VŒ‹‰Ê “ú–{Œê
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—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
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K214-P006 Elastic wave velocity measurements of Tanzawa hornblende gabbro up to 800 degrees C and 1.0GPa “ú–{Œê
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K214-P007 Elastic wave velocity measurement under high pressure and temperature conditions for lower crust rocks in the Kohistan arc “ú–{Œê
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—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
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—L‹g Œc‰î* J169-P011 ŠC’ê�E“àŠÏ‘ªƒf�[ƒ^‚ÉŠî‚­—]Œø‚·‚ׂè‰ß’ö‚Ì�„’è “ú–{Œê
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T225-001 ŠC�aŒ^‹�‘å’n�k�kŒ¹ˆæ‚ÌƒŠƒAƒ‹ƒ^ƒCƒ€ƒ‚ƒjƒ^ƒŠƒ“ƒO “ú–{Œê
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’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
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K132-007 Theoretical constraints on the origin of chloritite at the uppermost gabbro unit in the Oman ophiolite “ú–{Œê
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L215-001 “ñŽ_‰»’Y‘f‚Ì’n’†Œº•�Šâ‘w’™—¯‚ÉŠÖ‚·‚éŽÀŒ±“IŒ¤‹† “ú–{Œê
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R219-004 Discovery of the fourth deep-sea mineral resource “ú–{Œê
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R219-P001 �g‘æ4‚Ì�[ŠC’ê�z•¨Ž‘Œ¹�h‚̃|ƒeƒ“ƒVƒƒƒ‹•]‰¿ “ú–{Œê
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* R219-P002 A rapid and precise determination of rare metals in various types of deep-sea mineral resources by ICP-MS “ú–{Œê
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ˆÀ“¡ �Lˆê* S147-008 ’f‘w�š‹È‚Ì”­�¶�ðŒ�‚ƃ�ƒJƒjƒYƒ€�@-—§�ì’f‘w‚ðŽ–—á‚Æ‚µ‚Ä- “ú–{Œê
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ˆÀ“¡ ”E* D108-P020 ALOS/PALSAR‚É‚æ‚茟�o‚³‚ꂽƒjƒ…�[ƒMƒjƒA•t‹ß‚Ì’n�k‚É”º‚¤’nŠk•Ï“® “ú–{Œê
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* D109-P009 б�ÂSAR‰æ‘œ‚ł݂½‘S�‘‚ÌŠˆ‰ÎŽR�i‚Q�j “ú–{Œê
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V159-P014 ƒtƒBƒŠƒsƒ“�Cƒ}ƒˆƒ“‰ÎŽR‚É‚¨‚¯‚é—\”õ“I‚È’nŠk•Ï“®ŠÏ‘ª‚ɂ‚¢‚Ä “ú–{Œê
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ˆÀ“Œ �~ˆê* T223-013 ƒAƒ“ƒ`ƒSƒ‰ƒCƒgŽÖ–äŠâ‚Ì‘Y�«•ÏŒ`“Á�« “ú–{Œê
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T223-016 ’¾‚Ý�ž‚ݑтł̋­‚¢’n�k”gˆÙ•û�«‚ÍŽÖ–äŠâ‚É‚æ‚é�H “ú–{Œê
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T223-P006 ƒ}ƒ“ƒgƒ‹ƒEƒFƒbƒW�ðŒ�‚ł֖̎äŠâ‚Ì™’’f•ÏŒ`ŽÀŒ± “ú–{Œê
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ˆÀ“¡ —²Žu V159-026 2008”N�÷“‡�l�H’n�k’T�¸‚̃f�[ƒ^‚ð—p‚¢‚½P”g‘¬“x�\‘¢‰ð�Í “ú–{Œê
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* V159-P012 �l�H’n�k’T�¸‚É‚æ‚鈦—ǃJƒ‹ƒfƒ‰‚Ì�ó•”�\‘¢ “ú–{Œê
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ˆÀ“¡ �hŠî* P140-P014 �u‚©‚®‚â�vŽq‰q�¯‚Q‹@‚ð—p‚¢‚½ŒŽ‚Ì“d—£‘w‚Ì“d”g‰†•ÁŠÏ‘ª “ú–{Œê
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P144-023 ‚©‚®‚â“d”g‰ÈŠw‚É‚æ‚錎“d—£‘w‚ÌŠÏ‘ª “ú–{Œê
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ˆÀ“¡ �½ D106-008 ”\“o”¼“‡–k•”‰«‚É‚¨‚¯‚éŠC’ê�d—Í’²�¸ “ú–{Œê
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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
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ˆÀ“¡ ‰ë�F D108-004 ŠC’ê’nŠk•Ï“®Œv‘ª�¸“xŒü�ã‚Ì‚½‚߂̉ð�̓VƒXƒeƒ€OCDASAN‚̉ü’ù “ú–{Œê
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* D108-005 ‘ä˜p‚É‚¨‚¯‚éŠC’ê’nŠk•Ï“®ŠÏ‘ª “ú–{Œê
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J173-P018 ’†•”—®‹…ŠC�a‚ł̊C’ê’nŠk•Ï“®ŠÏ‘ª “ú–{Œê
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J173-P020 ƒWƒƒƒCƒ�‚ƃTƒeƒ‰ƒCƒgƒRƒ“ƒpƒX‚É‚æ‚éŠC’ê’nŠk•Ï“®‰ð�ÍŒ‹‰Ê‚̈Ⴂ “ú–{Œê
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S154-004 ’Ôg–ÚŒ‚�ØŒ¾‚É‚à‚Æ‚­2004”NƒXƒ}ƒgƒ‰-ƒAƒ“ƒ_ƒ}ƒ“’n�k‚É‚¨‚¯‚éƒXƒ}ƒgƒ‰“‡•t‹ß‚Ì’f‘wƒ‚ƒfƒ‹‚Ì�„’è “ú–{Œê
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S156-005 Low frequency earthquakes near western margin of the Ryukyu trench axis “ú–{Œê
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ˆÀ“¡ —º•ã I130-010 •²‘Ì‘w‚Ì�‚‘¬–€ŽCŽÀŒ± “ú–{Œê
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* S155-006 ‰ÎŽR‚É�Ƃ炳‚ꂽ“à—¤Šˆ’f‘w‚Ì�ªŒ³ “ú–{Œê
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T226-003 •ªŠò’f‘wŒ`�¬‚Ì—ÍŠw�F’è—Ê“I‰ð�͂ƃ‚ƒfƒ‹‰» “ú–{Œê
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ˆÀ•” —Sˆê V159-P024 ‰ÎŽRŠÏ‘ª—pŽ©‘–Ž®ƒZƒ“ƒT�[‚ÌŠJ”­ “ú–{Œê
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ˆÀŠÔ —¹ J172-P001 Geologic architectures, physical-mechanical properties and geochemistry of the eastern Nankai prism along the Tenryu Canyon “ú–{Œê
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